Form:CSDMS annual meeting: Difference between revisions

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<br>
<br>
=Registration=
=Registration=
Registration will open Mid January. <span style="font-size:1.2em;"><font color="red">Please don't register yet, we're in a testing phase right now.</font></span><br><br>
The online conference registration is a three step process:
The online conference registration is a three step process:
{|
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|width=400px valign=bottom|
{{#ifexist:User:{{CURRENTUSER}}|::{{#show:User:{{CURRENTUSER}} |? First name member}}, continue<br>with '''step 2'''|
{{#ifexist:User:{{CURRENTUSER}}|::{{#show:User:{{CURRENTUSER}} |? First name member}}, continue<br>with '''step 2'''|
::<span class="plainlinks">[{{server}}{{localurl:Special:Userlogin|returnto=Form:CSDMS_annual_meeting }} Log in]</span> (<font size="0.6">or [[Special:RequestAccount | create account]] for non-CSDMS members</font>) <font color="gray" size="0.6"><br>Forgot username? <span class="plainlinks">[http://csdms.colorado.edu/wiki/Search_username Search]</span> or email:[mailto:CSDMSweb@colorado.edu CSDMSweb@colorado.edu]</font>}}
::<span class="plainlinks">[{{server}}{{localurl:Special:Userlogin|returnto=Form:CSDMS_annual_meeting }} Log in]</span> (<font size="0.6">or [[Special:RequestAccount | create account]] for non-CSDMS members</font>) <font color="gray" size="0.6"><br>Forgot username? <span class="plainlinks">[https://csdms.colorado.edu/wiki/Search_username Search]</span> or email:[mailto:CSDMSweb@colorado.edu CSDMSweb@colorado.edu]</font>}}
|-
|-
|valign=bottom|
|valign=bottom|
::<big>'''Step 2'''</big>:
::<big>'''Step 2'''</big>:
::::* '''Register'''  
::::* '''Register'''
::::* '''Abstract submission'''
|valign=middle|
|valign=middle|
::{{#formlink:form=CSDMS_annual_meeting|link text=Start registration|link type=button|query string=namespace=Meeting|new window|namespace=Meeting}}
::{{#formlink:form=CSDMS_annual_meeting|link text=Start registration|link type=button|query string=namespace=Meeting|new window|namespace=Meeting}}
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::<big>'''Step 3'''</big>:
::<big>'''Step 3'''</big>:
::::* '''Academia or Government, registration fee: $200'''<br>
::::* '''Academia or Government, registration fee: $200''' ''(After April 1st: $300)''<br>
::::* '''Industry, registration fee: $1,500<br><font color="gray" size="0.6">''Third party website''</font>
::::* '''Industry, registration fee: $1,500 ''' ''(After April 1st: $1,600)''<br>
::::* '''Add $30 when joining pre-conference bootcamp'''<br><font color="gray" size="0.6">''Third party website''</font>
|valign=middle|
|valign=middle|
::<span class="plainlinks">[[image:Pay_button.png|link=https://www.regonline.com/csdmsmeeting2016]]</span>
::<span class="plainlinks">[[image:Pay_button.png|link=https://www.regonline.com/csdmsmeeting2016]]</span>
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==Keynote Speakers==
==Keynote Speakers==
As of now:<br>
As of now:<br>
{{Keynote-clinics
| name = Jean Braun
| affiliation = Institut des Sciences de la Terre, Universitaire de Grenoble
| participants =
| title = Links Between Mantle Convection, Tectonics, Erosion and Climate: Recent Model Developments and Results
| abstract = Plate tectonics is the primary process controlling the Earth’s surface topography. In recent years, geodynamicists have emphasised the role that deep mantle flow may play in directly creating long wavelength, low amplitude topography (a so-called “dynamic” contribution to surface topography). In parallel, geomorphologists have investigated how surface processes (erosion, transport and sedimentation) may affect dynamic topography, with the aim of better understanding its signature in the geological record. To achieve this, we have developed a new class of surface processes models that represent the combined effects of physical erosion and chemical alteration within continental interiors. In developing these models, we have paid much attention to maintaining high efficiency and stability such that they could be used to model large continental areas with sufficient spatial resolution to represent the processes at the appropriate scale. I will briefly present these algorithms as well as the results of two separate studies in which we explain the anomalously rapid erosion of surface material during the passage of a continent over a fixed source of dynamic topography driven by upward flow in the mantle. I will also comment on how these models are strongly dependent on precipitation patterns and, ultimately, will need to be fully coupled to climate models to provide more meaningful constraints on the past evolution of surface topography. <br>
}}
{{Keynote-clinics
| name = Enrique Curchitser
| affiliation = Institute of Marine and Coastal Sciences, Rutgers University
| participants =
| title = draft - Multi-Scale Modeling of Ocean Boundary Currents
| abstract =
}}
{{Keynote-clinics
| name = Mark Rounsevell
| affiliation = University of Edinburgh
| participants =
| title = draft - Integrative assessment modeling and Climate Change
| abstract =
}}
{{Keynote-clinics
{{Keynote-clinics
| name = Wonsuck Kim
| name = Wonsuck Kim
Line 71: Line 92:
| participants =  
| participants =  
| title = draft - Sediment Experimentalists Network Activities and Future Direction  
| title = draft - Sediment Experimentalists Network Activities and Future Direction  
| abstract = <br>
| abstract =  
}}
}}
{{Keynote-clinics
{{Keynote-clinics
| name = Jean Braun
| name = Jean-Francois Lamarque
| affiliation = Institut des Sciences de la Terre, Universitaire de Grenoble
| affiliation = National Center for Atmospheric Research
| participants =  
| participants =  
| title = Links Between Mantle Convection, Tectonics, Erosion and Climate: Recent Model Developments and Results
| title = draft - Community Earth System Model
| abstract = Plate tectonics is the primary process controlling the Earth’s surface topography. In recent years, geodynamicists have emphasised the role that deep mantle flow may play in directly creating long wavelength, low amplitude topography (a so-called “dynamic” contribution to surface topography). In parallel, geomorphologists have investigated how surface processes (erosion, transport and sedimentation) may affect dynamic topography, with the aim of better understanding its signature in the geological record. To achieve this, we have developed a new class of surface processes models that represent the combined effects of physical erosion and chemical alteration within continental interiors. In developing these models, we have paid much attention to maintaining high efficiency and stability such that they could be used to model large continental areas with sufficient spatial resolution to represent the processes at the appropriate scale. I will briefly present these algorithms as well as the results of two separate studies in which we explain the anomalously rapid erosion of surface material during the passage of a continent over a fixed source of dynamic topography driven by upward flow in the mantle. I will also comment on how these models are strongly dependent on precipitation patterns and, ultimately, will need to be fully coupled to climate models to provide more meaningful constraints on the past evolution of surface topography. <br>
| abstract =
}}
}}
{{Keynote-clinics
{{Keynote-clinics
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}}
}}
{{Keynote-clinics
{{Keynote-clinics
| name = Enrique Curchitser
| name = Bette Otto-Blisner
| affiliation = Institute of Marine and Coastal Sciences, Rutgers University
| affiliation = NCAR
| participants =  
| participants =  
| title = draft - Multi-Scale Modeling of Ocean Boundary Currents
| title = Draft: Continental Modeling
| abstract = <br>
| abstract =
}}
}}
{{Keynote-clinics
{{Keynote-clinics
| name = Jean-Francois Lamarque
| name = Jon Pelletier
| affiliation = National Center for Atmospheric Research
| affiliation = University of Arizona
| participants =  
| participants =  
| title = draft - Community Earth System Model
| title = Modeling the Impact of Vegetation Changes on Erosion Rates and Landscape Evolution
| abstract = <br>
| abstract = In landscape evolution models, climate change is often assumed to be synonymous with changes in rainfall. In many climate changes, however, the dominant driver of landscape evolution is changes in vegetation cover. In this talk I review case studies that attempt to quantify the impact of vegetation changes on landscape evolution, including examples from hillslope/colluvial, fluvial, and aolian environments, spatial scales of ~10 m to whole continents, and time scales from decadal to millennial. Particular attention is paid to how to parameterize models using paleoclimatic and remote sensing data. 
}}
}}
{{Keynote-clinics
{{Keynote-clinics
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| affiliation = Environmental CrossRoads Initiative, CUNY Advanced Science Research Center
| affiliation = Environmental CrossRoads Initiative, CUNY Advanced Science Research Center
| participants =  
| participants =  
| title = draft - Sea Level Changes
| title = From Relative Sea Level Rise to Coastal Risk: Estimating Contemporary and Future Flood Risk in Deltas
| abstract = <br>  
| abstract = Deltas are highly sensitive to local human activities, land subsidence, regional water management, global sea-level rise, and climate extremes.  In this talk, I’ll discuss a recently developed risk framework for estimating the sensitivity of deltas to relative sea level rise, and the expected impact on flood risk. We apply this framework to an integrated set of global environmental, geophysical, and social indicators over 48 major deltas to quantify how delta flood risk due to extreme events is changing over time.  Although geophysical and relative sea-level rise derived risks are distributed across all levels of economic development, wealthy countries effectively limit their present-day threat by gross domestic product–enabled infrastructure and coastal defense investments. However, when investments do not address the long-term drivers of land subsidence and relative sea-level rise, overall risk can be very sensitive to changes in protective capability. For instance, we show how in an energy-constrained future scenario, such protections will probably prove to be unsustainable, raising relative risks by four to eight times in the Mississippi and Rhine deltas and by one-and-a-half to four times in the Chao Phraya and Yangtze deltas. This suggests that the current emphasis on short-term solutions on the world’s deltas will greatly constrain options for designing sustainable solutions in the long term.
}}
{{Keynote-clinics
| name = Don Deangelis
| affiliation = USGS
| participants =
| title = Ecological Applications of Agent Based Models
| abstract =
}}<!---->
 
==Clinic Leaders==
===Tuesday (1<sup>st</sup> day)===
{{Keynote-clinics
| name = Irina Overeem & Mark Piper
| affiliation = CSDMS Integration Facility, INSTAAR, University of Colorado Boulder
| participants =
| title = Using TopoFlow in the classroom
| abstract = TopoFlow is a spatially distributed hydrologic model that includes meteorology, snow melt, evapotranspiration, infiltration and flow routing components. It can model many different physical processes in a watershed with the goal of accurately predicting how various hydrologic variables will evolve in time in response to climatic forcings. In the past year, CSDMS IF staff integrated TopoFlow into the CSDMS Web Modeling Tool (WMT, https://csdms.colorado.edu/wmt) and developed new lesson plans for use with it.<br><br>The first part of this clinic focuses on the technical aspects of working with TopoFlow in WMT, including how to: load and couple components, get information on a component, set parameters, upload data files, save a model, and run a model. We’ll discuss features of the TopoFlow implementation in WMT, and explain choices that were made in bringing TopoFlow to the web.<br><br>In the second part of the clinic, we’ll focus on science and education. We will run several TopoFlow simulations on the CSDMS HPCC through WMT. Participants will explore parameter settings, submit runs, and view netCDF output using NASA’s Panoply tool. <br><br>The learning outcomes of this clinic are to have better insight into the behavior of TopoFlow components, and the implementation of these in WMT. Participants will learn how to do TopoFlow model runs, and will have access to TopoFlow online labs and teaching resources lesson plans.
}}
{{Keynote-clinics
| name = Ehab Mesehle & Eric White
| affiliation = The Water Institute of the Gulf
| participants =
| title = Coastal Ecosystem Integrated Compartment Model (ICM): Modeling Framework
| abstract = The Integrated Compartment Model (ICM) was developed as part of the 2017 Coastal Master Plan modeling effort. It is a comprehensive and numerical hydrodynamic model coupled to various geophysical process models. Simplifying assumptions related to some of the flow dynamics are applied to increase the computational efficiency of the model.  The model can be used to provide insights about coastal ecosystems and evaluate restoration strategies. It builds on existing tools where possible and incorporates newly developed tools where necessary. It can perform decadal simulations (~ 50 years) across the entire Louisiana coast. It includes several improvements over the approach used to support the 2012 Master Plan, such as: additional processes in the hydrology, vegetation, wetland and barrier island morphology subroutines, increased spatial resolution, and integration of previously disparate models into a single modeling framework. The ICM includes habitat suitability indices (HSIs) to predict broad spatial patterns of habitat change, and it provides an additional integration to a dynamic fish and shellfish community model which quantitatively predicts potential changes in important fishery resources. It can be used to estimate the individual and cumulative effects of restoration and protection projects on the landscape, including a general estimate of water levels associated with flooding. The ICM is also used to examine possible impacts of climate change and future environmental scenarios (e.g. precipitation, Eustatic sea level rise, subsidence, tropical storms, etc.) on the landscape and on the effectiveness of restoration projects. The ICM code is publically accessible, and coastal restoration and protection groups interested in planning-level modeling are encouraged to explore its utility as a computationally efficient tool to examine ecosystem response to future physical or ecological changes, including the implementation of restoration and protection strategies.
}}
{{Keynote-clinics
| name = Mary Hill
| affiliation = University of Kansas
| participants =
| title = MODFLOW: Example applications and what we can learn from this amazingly successful piece of environmental modeling software.
| abstract =
}}
{{Keynote-clinics
| name = Scott Peckham and Allen Pope, University of Colorado, Boulder
| affiliation = USC, ISI
| participants =
| title = Geoscience Paper of the Future: Training Session on Best Practices for Publishing Your Research Products
| abstract = The Geoscience Paper of the Future (GPF) Initiative was created to encourage geoscientists to publish papers together with their associated digital research products following best practices of reproducible articles, open science, and digital scholarship.  A GPF includes: 1) Data available in a public repository, including metadata, a license specifying conditions of use, and a citation using a unique and persistent identifier; 2) Software available in a public repository, with documentation, a license for reuse, and a unique and citable using a persistent identifier; 3) Provenance of the results by explicitly describing method steps and their outcome in a workflow sketch, a formal workflow, or a provenance record. Learn to write a GPF and submit to a special section of AGU’s Earth and Space Sciences Journal.  More at http://www.ontosoft.org/gpf/.
}}
===Wednesday (2<sup>nd</sup> day)===
{{Keynote-clinics
| name = Wonsuck Kim
| affiliation = The University of Texas at Austin
| participants =
| title = SEN
| abstract =
}}
}}
{{Keynote-clinics
{{Keynote-clinics
| name = Jon Pelletier
| name = Eric Hutton & Mark Piper
| affiliation = University of Arizona
| affiliation = CSDMS Integration Facility, INSTAAR, University of Colorado Boulder
| participants =  
| participants =  
| title = Earth's Future - Landscape Response to Climate and Land-Use Change
| title = BMI: Live!
| abstract = <br>  
| abstract = CSDMS has developed the Basic Model Interface (BMI) to simplify the conversion of an existing model in C, C++, Fortran, Java, or Python into a reusable, plug-and-play component. By design, the BMI functions are straightforward to implement. However, in practice, the devil is in the details.<br><br>In this hands-on clinic, we will take a model -- in this case, an implementation of the two-dimensional heat equation in Python -- and together, we will write the BMI functions to transform it into a component. As we develop, we’ll unit test our component with nose, and we’ll explore how to use the component with a Jupyter Notebook. Optionally, we can set up a GitHub repository to store and to track changes to the code we write.<br><br>To get the most out of this clinic, come prepared to code! We have a lot to write in the time allotted. We recommend that clinic attendees have a laptop with the Anaconda Python distribution installed. We also request that you skim:<br><br>&#10501; BMI description (https://csdms.colorado.edu/wiki/BMI_Description)<br>&#10501; BMI documentation (http://bmi-forum.readthedocs.org/en/latest)<br><br>before participating in the clinic.
}}<!--
}}
{{Keynote-clinics
{{Keynote-clinics
| name =  
| name = Courtney Harris, Julia Moriarty & Irina Overeem and Eric Hutton
| affiliation =
| affiliation = VIMS & Univ. of Colorado
| participants =  
| participants =  
| title =  
| title = Regional Ocean Modeling System (ROMS): An introductory web-based model implementation
| abstract = <br>  
| abstract = Participants in this clinic will learn how to run a Regional Ocean Modeling System (ROMS) test case for an idealized continental shelf model domain within the CSDMS Web Modeling Toolkit (WMT). The model implementation that we will use includes wave forcing, a riverine source, suspended sediment transport.<br><br>ROMS is an open source, three-dimensional primitive equation hydrodynamic ocean model that uses a structured curvilinear horizontal grid and a stretched terrain following vertical grid. For more information see https://www.myroms.org. It currently has more than 4,000 registered users, and the full model includes modules for sediment transport and biogeochemistry, and several options for turbulence closures and numerical schemes. In part because ROMS was designed to provide flexibility for the choice of model parameterizations and processes, and to run in parallel, implementing the code can seem daunting, but in this clinic, we will present an idealized ROMS model that can be run on the CSDMS cluster via the WMT.  One goal is to provide a relatively easy introduction to the numerical modeling process that can be used within upper level undergraduate and graduate classes to explore sediment transport on continental shelves.<br><br>As a group, we will run an idealized ROMS model on the CSDMS computer, Beach. The group will choose a modification to the standard model. While the modified model runs, we will explore methods for visualizing model output. Participants who have access to WMT can run the model themselves. Clinic participants who have access to Matlab and/or Panoply will be able to browse model output files during the clinic.<br><br>Following the clinic, participants should have access to an example ROMS model run, experience running ROMS within the WMT and with ROMS input and output files, and. ROMS lesson plans.
}}-->
}}
 
==Clinic Leaders==
As of now:<br>
<!--===Tuesday (1<sup>st</sup> day)===-->
{{Keynote-clinics
{{Keynote-clinics
| name = Zheyu Zhou, Xiaofeng Liu & Tom Hsu
| name = Zheyu Zhou, Xiaofeng Liu & Tom Hsu
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| abstract =
| abstract =
}}
}}
===Thursday (3<sup>rd</sup> day)===
{{Keynote-clinics
{{Keynote-clinics
| name = Mark Piper & Eric Hutton
| name = Greg Tucker
| affiliation = CSDMS, University of Colorado
| affiliation = CIRES, Univ. of Colorado
| participants =  
| participants =  
| title = WMT and the Dakota iterative systems toolkit
| title = LandLab
| abstract = Dakota (https://dakota.sandia.gov) is an open-source software toolkit, designed and developed at Sandia National Laboratories, that provides a library of iterative systems analysis methods, including sensitivity analysis, uncertainty quantification, optimization, and parameter estimation. Dakota can be used to answer questions such as:<br><br>·What are the important parameters in my model?<br>·How safe, robust, and reliable is my model?<br>·What parameter values best match my observational data?<br><br>Dakota has been installed on the CSDMS supercomputer, beach, and is available to all registered users. The full set of Dakota methods can be invoked from the command line on beach; however, this requires detailed knowledge of Dakota, including how to set up a Dakota input file, and how to pass parameters and responses between a model and Dakota. To make Dakota more accessible to the CSDMS community, a subset of its functionality has been configured to run through the CSDMS Web Modeling Tool (WMT; https://csdms.colorado.edu/wmt). WMT provides access to the following Dakota methods:<br><br>·vector, centered, list and multidimensional parameter studies<br>·design and analysis of computer experiments with Monte Carlo and Latin Hypercube sampling methods<br>·uncertainty quantification with sampling, polynomial chaos expansion and stocastic collocation techniques<br><br>In this clinic, we'll provide an overview of Dakota, then, through WMT, set up and perform a series of numerical experiments with Dakota on beach, and evaluate the results.<br>
| abstract =
}}
}}
<!--===Wednesday (2<sup>nd</sup> day)===-->
<!--
{{Keynote-clinics
{{Keynote-clinics
| name = Eric Hutton & Mark Piper
| name = --
| affiliation = CSDMS, University of Colorado
| affiliation =  
| participants =  
| participants =  
| title =Wrapping Existing Models with the Basic Modeling Interface
| title = Numpy
| abstract = In order to simplify conversion of an existing model to a reusable, plug-and-play model component, CSDMS has developed a simple interface called the Basic Model Interface (BMI) that model developers are asked to implement. In this context, an interface is a named set of functions with prescribed function names, argument types and return types. By design, the BMI functions are straightforward to implement in C, C++, Fortran, Java and Python. Also by design, the BMI functions are noninvasive. A BMI-compliant model does not make any calls to CSDMS components or tools and is not modified to use CSDMS data structures. BMI therefore introduces no dependencies into a model and the model can still be used in a stand-alone manner.<br><br>Models that provide a BMI can be incorporated into a modeling framework, such as the CSDMS model coupling framework, where they gain new capabilities provided by the framework. The CSDMS framework allows coupling of models even if they differ in:<br><br>• programming language,<br>• variable names,<br>• variable units,<br>• time-stepping scheme or<br>• computational grid is different.<br><br>Framework models also gain the ability to write output variables to NetCDF files, a graphical user interface, and the ability to run within the CSDMS Web Tool.<br><br>This clinic will explain the key concepts of BMI (and CSDMS Standard Names), and will demonstrate, through example, how to implement a BMI for an existing model. It will also include an overview of the CSDMS Standard Names, which provide a uniform way to map input and output variable names between component models as part of a BMI implementation. Participants are encouraged to read the associated CSDMS wiki pages in advance. See<br><br>• [[BMI_Description|BMI Description]]<br>• [[CSDMS_Standard_Names|CSDMS Standard Names]]
| abstract =
}}-->
}}


<!--===Thursday (3<sup>rd</sup> day)===-->
{{Keynote-clinics
{{Keynote-clinics
| name = Irina Overeem & Mark Piper
| name = Wei Luo
| affiliation = CSDMS, University of Colorado
| affiliation = Northern Illinois University
| participants =  
| participants =  
| title = Bringing CSDMS Models into the Classroom
| title = WILSIM as EKT tool
| abstract = CSDMS has developed a Web-based Modeling Tool – the WMT. WMT allows users to select models, to edit model parameters, and run the model on the CSDMS High-Performance Computing System.  The web interface makes it straightforward to configure different model components and run a coupled model simulation. Users can monitor progress of simulations and download model output.<br><br> CSDMS has developed educational labs that use the WMT to teach quantitative concepts in geomorphology, hydrology, coastal evolution. These labs are intended to be used by Teaching assistants and Faculty alike. Descriptions of 4-hr hands-on labs have been developed for HydroTrend, Plume, Sedflux, CHILD, ERODE and ROMS-Lite. These labs include instructions for students to run the models and explore dominant parameters in sets of simulations.  Learning objectives are split between topical concepts, on climate change and sediment transport amongst many others, and modeling strategies, modeling philosophy and critical assessment of model results.<br><br>In this clinic, we will provide an overview of the available models and labs, and their themes and active learning objectives. We will discuss the requirements  and logistics of using the WMT in your classroom. We will run some simulations hands-on, and walk through one lab in more detail as a demonstration. Finally, the workshop intends to discuss future developments for undergraduate course use with the participants.
| abstract =
}}
}}
{{Keynote-clinics
{{Keynote-clinics
| name = Greg Tucker
| name = Randy LeVeque
| affiliation = CIRES, University of Colorado
| affiliation = University of Washington, Seattle
| participants =  
| participants =  
| title = Landlab: A Python library for building, exploring, and coupling 2D surface-process models
| title = GeoClaw Software for Depth Average Flow
| abstract = Gregory E. Tucker <sup>1</sup>, Daniel E.J. Hobley <sup>1</sup>, Jordan M. Adams <sup>2</sup>, Sai S. Nudurupati <sup>3</sup>, Eric Hutton <sup>4</sup>, Nicole M. Gasparini <sup>2</sup>, and Erkan Istanbulluoglu <sup>3</sup><br><br><small><sup>1</sup> CIRES and Department of Geological Sciences, University of Colorado at Boulder<br><sup>2</sup> Department of Earth and Environmental Sciences, Tulane University<br><sup>3</sup> Department of Civil and Environmental Engineering, University of Washington<br><sup>4</sup> CSDMS, University of Colorado at Boulder</small><br><br>Writing the software to implement a two-dimensional numerical model can be a daunting exercise, even when the underlying discretization and numerical schemes are relatively simple. The challenge is even greater when the desired model includes ``advanced'' features such as an unstructured grid, a staggered-grid numerical solver, or input/output operations on gridded data. Landlab is a Python-language programming library that makes the process of 2D model-building simpler and more efficient. Landlab's core features include: (1) a gridding engine that lets you create and configure a structured or unstructured grid in just a few lines of code, and to attach data directly to the grid; (2) a library of pre-built process components that saves you from having to re-invent the wheel with common geoscience algorithms (such as flow routing on gridded terrain, linear and nonlinear diffusion, and elastic plate flexure); (3) a mechanism for coupling components together to create integrated model; and (4) a suite of tools for input/output and other common operations. Although Landlab's components are primarily related to earth-surface dynamics (including geomorphology and hydrology), its basic framework is applicable to many types of geophysical system. This clinic provides a hands-on tutorial introduction to Landlab. Participants will learn about Landlab's capabilities, and how to use it to build and run simple 2D models. Familiarity with the Python language and the Numpy library is helpful but not critical.
| abstract = GeoClaw (http://www.geoclaw.org) is an open-source software package for solving two-dimensional depth-averaged equations over general topography using high-resolution finite volume methods and adaptive mesh refinement. Wetting-and-drying algorithms allow modeling inundation or overland flows. The primary applications where GeoClaw has been used are tsunami modeling and storm surge, although it has also been applied to dam break floods and it forms the basis for the debris flow and landslide code D-Claw under development at the USGS Cascades Volcano Observatory.<br><br>This tutorial will give an introduction to setting up a tsunami modeling problem in GeoClaw including:<br>&#10501; Overview of capabilities,<br>&#10501; Installing the software,<br>&#10501; Using Python tools provided in GeoClaw to acquire and work with topography datasets and earthquake source models,<br>&#10501; Setting run-time parameters, including specifying adaptive refinement regions,<br>&#10501; Options to output snapshots of the solution or maximum flow depths, arrival times, etc.<br>&#10501; The VisClaw plotting software to visualize results using Python tools or display on Google Earth.<br><br>GeoClaw is distributed as part of Clawpack (http://www.clawpack.org), and available via the CSDMS model repository. Those who wish to install the software in advance on laptops, please see http://www.clawpack.org/installing.html.
}}
}}
<br><br>
<br><br>
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*[[CSDMS_meeting_2015_participant_list|Participants meeting]]
*[[CSDMS_meeting_2015_participant_list|Participants meeting]]
*[[CSDMS_meeting_2015_abstract_list|Submitted abstracts]]
*[[CSDMS_meeting_2015_abstract_list|Submitted abstracts]]
* Participants bootcamp
<br>
<br>
*[[CSDMS_pre-meeting_bootcamp|Participants bootcamp]] May 16<sup>th</sup>
<br><br>


=Reimbursement =
=Reimbursement =
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'''Note:'''
'''Note:'''
* Registration is open till April 1<sup>st</sup> (or until program fill) and is handled through the 2016 meeting site.<br>
* Registration is open till April 1<sup>st</sup> (or until program fill) and is handled through the 2016 meeting site.<br>
* The bootcamp is capped at 30 participants (first paid first serve), and it has a $25 registration fee.
* The bootcamp is capped at 30 participants (first paid first serve), and it has a $30 registration fee.
* Participant will be responsible for cost / organization of their extra day of hotel accommodation and dinner. Costs will not be reimbursed.
* Participant will be responsible for cost / organization of their extra day of hotel accommodation and dinner. Costs will not be reimbursed.
* We will cover coffee and lunch during the bootcamp.
* We will cover coffee and lunch during the bootcamp.
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* '''January 15<sup>th</sup>''': Registration opens
* '''January 15<sup>th</sup>''': Registration opens
* '''March 1<sup>st</sup>''': Deadline for student scholarship applications
* '''March 1<sup>st</sup>''': Deadline for student scholarship applications
* '''April 1<sup>st</sup>''': Deadline for abstract submission & registration
* '''April 1<sup>st</sup>''': Deadline for abstract submission & early registration
* '''May 10<sup>th</sup>''': Deadline late registration. ''Notice additional costs do apply.''
<!--* '''April 15<sup>th</sup>: Extended deadline for abstract submission & registration-->
<!--* '''April 15<sup>th</sup>: Extended deadline for abstract submission & registration-->
*  '''May 16<sup>th</sup>''': <font color="red">Optional</font>: pre-conference bootcamp
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'''<sup>*</sup>'''  ''The Sediment Experimentalist Network (SEN) integrates the efforts of sediment experimentalists to build a knowledge base for guidance on best practices for data collection and management. The network facilitates cross-institutional collaborative experiments and communicates with the research community about data and metadata guidelines for sediment-based experiments. This effort aims to improve the efficiency and transparency of sedimentary research for field geologists and modelers as well as experimentalists.''
'''<sup>*</sup>'''  ''The Sediment Experimentalist Network (SEN) integrates the efforts of sediment experimentalists to build a knowledge base for guidance on best practices for data collection and management. The network facilitates cross-institutional collaborative experiments and communicates with the research community about data and metadata guidelines for sediment-based experiments. This effort aims to improve the efficiency and transparency of sedimentary research for field geologists and modelers as well as experimentalists.''
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== Registration form ==
<center><big>CSDMS Meeting 2015<br> '''Models meet Data, Data meet Models'''</big></center><br><br>
<center><big>Joint CSDMS - SEN Meeting 2016<br> '''Capturing Climate Change'''</big></center><br><br>
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|All submitted registrations will be reviewed by a CSDMS program committee. <br>
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|Please direct all inquiries to Lauren Borkowski: [mailto:csdms@colorado.edu csdms@colorado.edu] with subject title: "CSDMS Meeting 2015"
|Please direct all inquiries to Lynn McCready: [mailto:csdms@colorado.edu csdms@colorado.edu] with subject title: "Joint CSDMS - SEN Meeting 2016"
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'''Note''': ''This is only an indication that you would like to apply for the CSDMS offered student scholarships. See the meeting site to actually apply for the CSDMS student scholarships: [https://csdms.colorado.edu/wiki/Form:CSDMS_annual_meeting#Student_Scholarships_(two_options)]''
</div>
<div id="scholarship_SEN">
'''Note''': ''This is only an indication that you would like to apply for the SEN offered scholarships. See the meeting site to actually apply for the SEN student scholarships: [https://csdms.colorado.edu/wiki/Form:CSDMS_annual_meeting#Student_Scholarships_(two_options)]''
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{| class="formtable"
| valign=top style="width:300px;"|Join the pre-conference meeting:
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'''Note''': ''Pre-Conference is an one day event, May 16<sup>th</sup> and will '''cost an additional $30'''. No reimbursement will be provided for extra night hotel or dinner.''
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| valign=top colspan="2"| <br><font color="gray">''Help us schedule the meeting! Select for each day the clinic you would like to attend:''<br>''(See [http://csdms.colorado.edu/wiki/Form:CSDMS_annual_meeting#Clinic_Invitees Clinics] for more information)''</font><br><br>
| valign=top colspan="2"| <br><font color="gray">''Help us schedule the meeting! Select for each day the clinic you would like to attend:''<br>''(See [https://csdms.colorado.edu/wiki/Form:CSDMS_annual_meeting#Clinic_Leaders clinic leaders] for more information)''</font><br><br>
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| valign=top style="width:300px;"|Select <b>one clinic</b> for the 1<sup>st</sup> day<br>(<i>Parallel sessions</i>):
| valign=top style="width:300px;"|Select <b>one clinic</b> for the 1<sup>st</sup> day<br>(<i>Parallel sessions</i>):
| valign=top |{{{field|CSDMS_meeting_select_clinics1|mandatory|input type=dropbox|default = 1) WMT and Dakota iterative toolkit}}}
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| valign=top style="width:300px;"|Select <b>one clinic</b> for the 2<sup>nd</sup> day<br>(<i>Parallel sessions</i>):
| valign=top |{{{field|CSDMS_meeting_select_clinics2|mandatory|input type=dropbox|default=1) Coastal Evolution Modeling (CEM)}}}
| valign=top |{{{field|CSDMS_meeting_select_clinics2|mandatory|input type=dropbox|default=1) SEN}}}
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| valign=top style="width:300px;"|Select <b>one clinic</b> for the 3<sup>rd</sup> day<br>(<i>Parallel sessions</i>):
| valign=top |{{{field|CSDMS_meeting_select_clinics3|mandatory|input type=dropbox|default=1) Bringing CSDMS to the Classroom}}}
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Latest revision as of 17:16, 19 February 2018

The joint 2016 CSDMS - SEN* Annual Meeting
Capturing Climate Change


May 17 -19th 2016, Boulder Colorado, USA



Optional: May 16th 2016, pre-conference bootcamp


Registration

The online conference registration is a three step process:

Step 1:
  • Log in
Log in (or create account for non-CSDMS members)
Forgot username? Search or email:CSDMSweb@colorado.edu
Step 2:
  • Register
  • Abstract submission
Step 3:
  • Academia or Government, registration fee: $200 (After April 1st: $300)
  • Industry, registration fee: $1,500 (After April 1st: $1,600)
  • Add $30 when joining pre-conference bootcamp
    Third party website
Pay button.png

Note 1: You only are successfully registered by fulfilling the above steps
Note 2: Do you want to make changes to you abstract?

  1. Log in.
  2. Select your registration record in "participants" and start making changes by clicking "Edit registration".




Objectives and general description

The joint CSDMS - SEN* 2016 annual meeting will focus on “advances in simulating the imprint of climate change on the land and seascapes, including the processes that influence them”. We would like presentations to either focus on the impacts of present and future climate change, or how climate change has impacted the earth in the past. Topics of interests also include modeling research that integrate different disciplines, different scales, and the synergy between models and experimental data. As in past meetings, keynote speakers are by invitation only, and poster presentations are the general media. The meeting will include:

  1. State-of-the art keynote presentations in earth-surface dynamics and modeling
  2. Hands-on clinics related to community models, tools and approaches
  3. Transformative software products and approaches designed to be accessible, easy to use, and relevant
  4. Breakout sessions for Working, Focus Research Groups and the Initiatives
  5. Poster Sessions

and more!

Poster Information: The poster boards are configured for 4' wide by 6' tall (portrait orientation) posters. The deadline to submit abstracts is April 15, 2016.

Agenda

Click here to view the draft agenda of 12/29/2015.

Keynote Speakers

As of now:

Jean Braun
Institut des Sciences de la Terre, Universitaire de Grenoble
Links Between Mantle Convection, Tectonics, Erosion and Climate: Recent Model Developments and Results
Plate tectonics is the primary process controlling the Earth’s surface topography. In recent years, geodynamicists have emphasised the role that deep mantle flow may play in directly creating long wavelength, low amplitude topography (a so-called “dynamic” contribution to surface topography). In parallel, geomorphologists have investigated how surface processes (erosion, transport and sedimentation) may affect dynamic topography, with the aim of better understanding its signature in the geological record. To achieve this, we have developed a new class of surface processes models that represent the combined effects of physical erosion and chemical alteration within continental interiors. In developing these models, we have paid much attention to maintaining high efficiency and stability such that they could be used to model large continental areas with sufficient spatial resolution to represent the processes at the appropriate scale. I will briefly present these algorithms as well as the results of two separate studies in which we explain the anomalously rapid erosion of surface material during the passage of a continent over a fixed source of dynamic topography driven by upward flow in the mantle. I will also comment on how these models are strongly dependent on precipitation patterns and, ultimately, will need to be fully coupled to climate models to provide more meaningful constraints on the past evolution of surface topography.
Enrique Curchitser
Institute of Marine and Coastal Sciences, Rutgers University
draft - Multi-Scale Modeling of Ocean Boundary Currents
Mark Rounsevell
University of Edinburgh
draft - Integrative assessment modeling and Climate Change
Wonsuck Kim
University of Texas
draft - Sediment Experimentalists Network Activities and Future Direction
Jean-Francois Lamarque
National Center for Atmospheric Research
draft - Community Earth System Model
Nikki Lovenduski
Department of Atmospheric and Ocean Sciences and Institute of Arctic and Alpine Research, University of Colorado, Boulder
Ocean Carbon Uptake and Acidification: Can We Predict the Future?
The oceans have absorbed a large fraction of anthropogenic carbon dioxide emissions, having consequences for ocean biogeochemistry and ecosystems via ocean acidification. Simulations with Earth System Models can be used to predict the future evolution of ocean carbon uptake and acidification in the coming decades and beyond, but there is substantial uncertainty in these model predictions, particularly on regional scales. Such uncertainty challenges decision makers faced with protecting the future health of ocean ecosystems. Uncertainty can be separated into three component parts: (1) uncertainty due to internal variability, (2) uncertainty due to model structure, and (3) uncertainty due to emission scenario. Here, we isolate and quantify the evolution of these three sources of prediction uncertainty in ocean carbon uptake over the next century using output from two sets of ensembles from the Community Earth System Model (CESM) along with output from models participating in the Fifth Coupled Model Intercomparison Project (CMIP5). We find that the three sources of prediction uncertainty in ocean carbon uptake are not constant, but instead vary with prediction lead time and the scale of spatial averaging. In order to provide valuable predictions to decision makers, we should invest in reducing the main sources of uncertainty.
Bette Otto-Blisner
NCAR
Draft: Continental Modeling
Jon Pelletier
University of Arizona
Modeling the Impact of Vegetation Changes on Erosion Rates and Landscape Evolution
In landscape evolution models, climate change is often assumed to be synonymous with changes in rainfall. In many climate changes, however, the dominant driver of landscape evolution is changes in vegetation cover. In this talk I review case studies that attempt to quantify the impact of vegetation changes on landscape evolution, including examples from hillslope/colluvial, fluvial, and aolian environments, spatial scales of ~10 m to whole continents, and time scales from decadal to millennial. Particular attention is paid to how to parameterize models using paleoclimatic and remote sensing data.
Zach Tessler
Environmental CrossRoads Initiative, CUNY Advanced Science Research Center
From Relative Sea Level Rise to Coastal Risk: Estimating Contemporary and Future Flood Risk in Deltas
Deltas are highly sensitive to local human activities, land subsidence, regional water management, global sea-level rise, and climate extremes. In this talk, I’ll discuss a recently developed risk framework for estimating the sensitivity of deltas to relative sea level rise, and the expected impact on flood risk. We apply this framework to an integrated set of global environmental, geophysical, and social indicators over 48 major deltas to quantify how delta flood risk due to extreme events is changing over time. Although geophysical and relative sea-level rise derived risks are distributed across all levels of economic development, wealthy countries effectively limit their present-day threat by gross domestic product–enabled infrastructure and coastal defense investments. However, when investments do not address the long-term drivers of land subsidence and relative sea-level rise, overall risk can be very sensitive to changes in protective capability. For instance, we show how in an energy-constrained future scenario, such protections will probably prove to be unsustainable, raising relative risks by four to eight times in the Mississippi and Rhine deltas and by one-and-a-half to four times in the Chao Phraya and Yangtze deltas. This suggests that the current emphasis on short-term solutions on the world’s deltas will greatly constrain options for designing sustainable solutions in the long term.
Don Deangelis
USGS
Ecological Applications of Agent Based Models

Clinic Leaders

Tuesday (1st day)

Irina Overeem & Mark Piper
CSDMS Integration Facility, INSTAAR, University of Colorado Boulder
Using TopoFlow in the classroom
TopoFlow is a spatially distributed hydrologic model that includes meteorology, snow melt, evapotranspiration, infiltration and flow routing components. It can model many different physical processes in a watershed with the goal of accurately predicting how various hydrologic variables will evolve in time in response to climatic forcings. In the past year, CSDMS IF staff integrated TopoFlow into the CSDMS Web Modeling Tool (WMT, https://csdms.colorado.edu/wmt) and developed new lesson plans for use with it.

The first part of this clinic focuses on the technical aspects of working with TopoFlow in WMT, including how to: load and couple components, get information on a component, set parameters, upload data files, save a model, and run a model. We’ll discuss features of the TopoFlow implementation in WMT, and explain choices that were made in bringing TopoFlow to the web.

In the second part of the clinic, we’ll focus on science and education. We will run several TopoFlow simulations on the CSDMS HPCC through WMT. Participants will explore parameter settings, submit runs, and view netCDF output using NASA’s Panoply tool.

The learning outcomes of this clinic are to have better insight into the behavior of TopoFlow components, and the implementation of these in WMT. Participants will learn how to do TopoFlow model runs, and will have access to TopoFlow online labs and teaching resources lesson plans.
Ehab Mesehle & Eric White
The Water Institute of the Gulf
Coastal Ecosystem Integrated Compartment Model (ICM): Modeling Framework
The Integrated Compartment Model (ICM) was developed as part of the 2017 Coastal Master Plan modeling effort. It is a comprehensive and numerical hydrodynamic model coupled to various geophysical process models. Simplifying assumptions related to some of the flow dynamics are applied to increase the computational efficiency of the model. The model can be used to provide insights about coastal ecosystems and evaluate restoration strategies. It builds on existing tools where possible and incorporates newly developed tools where necessary. It can perform decadal simulations (~ 50 years) across the entire Louisiana coast. It includes several improvements over the approach used to support the 2012 Master Plan, such as: additional processes in the hydrology, vegetation, wetland and barrier island morphology subroutines, increased spatial resolution, and integration of previously disparate models into a single modeling framework. The ICM includes habitat suitability indices (HSIs) to predict broad spatial patterns of habitat change, and it provides an additional integration to a dynamic fish and shellfish community model which quantitatively predicts potential changes in important fishery resources. It can be used to estimate the individual and cumulative effects of restoration and protection projects on the landscape, including a general estimate of water levels associated with flooding. The ICM is also used to examine possible impacts of climate change and future environmental scenarios (e.g. precipitation, Eustatic sea level rise, subsidence, tropical storms, etc.) on the landscape and on the effectiveness of restoration projects. The ICM code is publically accessible, and coastal restoration and protection groups interested in planning-level modeling are encouraged to explore its utility as a computationally efficient tool to examine ecosystem response to future physical or ecological changes, including the implementation of restoration and protection strategies.
Mary Hill
University of Kansas
MODFLOW: Example applications and what we can learn from this amazingly successful piece of environmental modeling software.
Scott Peckham and Allen Pope, University of Colorado, Boulder
USC, ISI
Geoscience Paper of the Future: Training Session on Best Practices for Publishing Your Research Products
The Geoscience Paper of the Future (GPF) Initiative was created to encourage geoscientists to publish papers together with their associated digital research products following best practices of reproducible articles, open science, and digital scholarship. A GPF includes: 1) Data available in a public repository, including metadata, a license specifying conditions of use, and a citation using a unique and persistent identifier; 2) Software available in a public repository, with documentation, a license for reuse, and a unique and citable using a persistent identifier; 3) Provenance of the results by explicitly describing method steps and their outcome in a workflow sketch, a formal workflow, or a provenance record. Learn to write a GPF and submit to a special section of AGU’s Earth and Space Sciences Journal. More at http://www.ontosoft.org/gpf/.

Wednesday (2nd day)

Wonsuck Kim
The University of Texas at Austin
SEN
Eric Hutton & Mark Piper
CSDMS Integration Facility, INSTAAR, University of Colorado Boulder
BMI: Live!
CSDMS has developed the Basic Model Interface (BMI) to simplify the conversion of an existing model in C, C++, Fortran, Java, or Python into a reusable, plug-and-play component. By design, the BMI functions are straightforward to implement. However, in practice, the devil is in the details.

In this hands-on clinic, we will take a model -- in this case, an implementation of the two-dimensional heat equation in Python -- and together, we will write the BMI functions to transform it into a component. As we develop, we’ll unit test our component with nose, and we’ll explore how to use the component with a Jupyter Notebook. Optionally, we can set up a GitHub repository to store and to track changes to the code we write.

To get the most out of this clinic, come prepared to code! We have a lot to write in the time allotted. We recommend that clinic attendees have a laptop with the Anaconda Python distribution installed. We also request that you skim:

⤅ BMI description (https://csdms.colorado.edu/wiki/BMI_Description)
⤅ BMI documentation (http://bmi-forum.readthedocs.org/en/latest)

before participating in the clinic.
Courtney Harris, Julia Moriarty & Irina Overeem and Eric Hutton
VIMS & Univ. of Colorado
Regional Ocean Modeling System (ROMS): An introductory web-based model implementation
Participants in this clinic will learn how to run a Regional Ocean Modeling System (ROMS) test case for an idealized continental shelf model domain within the CSDMS Web Modeling Toolkit (WMT). The model implementation that we will use includes wave forcing, a riverine source, suspended sediment transport.

ROMS is an open source, three-dimensional primitive equation hydrodynamic ocean model that uses a structured curvilinear horizontal grid and a stretched terrain following vertical grid. For more information see https://www.myroms.org. It currently has more than 4,000 registered users, and the full model includes modules for sediment transport and biogeochemistry, and several options for turbulence closures and numerical schemes. In part because ROMS was designed to provide flexibility for the choice of model parameterizations and processes, and to run in parallel, implementing the code can seem daunting, but in this clinic, we will present an idealized ROMS model that can be run on the CSDMS cluster via the WMT. One goal is to provide a relatively easy introduction to the numerical modeling process that can be used within upper level undergraduate and graduate classes to explore sediment transport on continental shelves.

As a group, we will run an idealized ROMS model on the CSDMS computer, Beach. The group will choose a modification to the standard model. While the modified model runs, we will explore methods for visualizing model output. Participants who have access to WMT can run the model themselves. Clinic participants who have access to Matlab and/or Panoply will be able to browse model output files during the clinic.

Following the clinic, participants should have access to an example ROMS model run, experience running ROMS within the WMT and with ROMS input and output files, and. ROMS lesson plans.
Zheyu Zhou, Xiaofeng Liu & Tom Hsu
Univ. Delaware, Penn State, Univ. Delaware,
Modeling coastal processes using OpenFOAM

Thursday (3rd day)

Greg Tucker
CIRES, Univ. of Colorado
LandLab
--

Numpy
Wei Luo
Northern Illinois University
WILSIM as EKT tool
Randy LeVeque
University of Washington, Seattle
GeoClaw Software for Depth Average Flow
GeoClaw (http://www.geoclaw.org) is an open-source software package for solving two-dimensional depth-averaged equations over general topography using high-resolution finite volume methods and adaptive mesh refinement. Wetting-and-drying algorithms allow modeling inundation or overland flows. The primary applications where GeoClaw has been used are tsunami modeling and storm surge, although it has also been applied to dam break floods and it forms the basis for the debris flow and landslide code D-Claw under development at the USGS Cascades Volcano Observatory.

This tutorial will give an introduction to setting up a tsunami modeling problem in GeoClaw including:
⤅ Overview of capabilities,
⤅ Installing the software,
⤅ Using Python tools provided in GeoClaw to acquire and work with topography datasets and earthquake source models,
⤅ Setting run-time parameters, including specifying adaptive refinement regions,
⤅ Options to output snapshots of the solution or maximum flow depths, arrival times, etc.
⤅ The VisClaw plotting software to visualize results using Python tools or display on Google Earth.

GeoClaw is distributed as part of Clawpack (http://www.clawpack.org), and available via the CSDMS model repository. Those who wish to install the software in advance on laptops, please see http://www.clawpack.org/installing.html.



Participants

Interested to see who registered for the meeting as of 05/18/2024?




Reimbursement

4878178960 fe558ee9b0 o TEDxBoulder.jpg

Within its budget, CSDMS intends to support member applicants to attend the annual meeting. Towards this goal, we encourage members to fully or partially cover their expenses if capable. We additionally thank those in the industry and agency fields for understanding that 1) we cannot compensate federal agency participants since our own funding is from NSF, and 2) we request that our industrial/ corporate participants cover their own costs thereby allowing more academic participants to attend.

To the extent possible, CSDMS intends to reimburse the registration fee, lodging (shared rooms at 100% and single rooms at 50% at conference hotels), and a limited amount of travel expenses for qualified registrants - those members who will attend all three days of the meeting and are not industry or federal employees.

Important for foreign travelers requesting reimbursement: If you need a visa to travel to USA, select a business visa. If you need an invitation letter, please email csdms@colorado.edu as soon as possible. Also indicate whether specific wording is required in the letter. Second, we will need to copy the entry stamp in your passport sometime during the meeting as proof that you were here on business as required by US tax laws for reimbursement (especially when dealing with airfare.) We are only able to provide reimbursement for airfare within the U.S. All airfare that is being reimbursed must be for airlines that are U.S. flag carriers.

Travel, Lodging and Conference Center Information

The meeting will be held at SEEC
Hotel: Millennium Harvest House Hotel
Transportation: You can book transportation between DIA and Boulder here: Green Ride Boulder. And information on how to find Green Ride Boulder at DIA.
We will provide a bus between the hotels and the meeting venue each day. We will also provide transportation to the banquet.

Pre-conference one-day Software Carpentry bootcamp

Boots.gif

CSDMS will host a Pre-conference one-day Software Carpentry bootcamp on Monday May 16th, 2016. The objective is to teach basic programming skills that will be useful for scientific computing and model development. This is an intensive, hands-on workshop, during which certified instructors will cover basic elements of:

  1. the Unix bash shell,
  2. Python programming and NumPy, and
  3. Github for version control.

Our instructors are earth scientists and have familiarity with the CSDMS framework, such that lessons and examples will be targeted toward relevant problems in your field. The bootcamp intentionally precedes the CSDMS meeting, so the skills participants develop should be useful in the clinics during the meeting.

Note:

  • Registration is open till April 1st (or until program fill) and is handled through the 2016 meeting site.
  • The bootcamp is capped at 30 participants (first paid first serve), and it has a $30 registration fee.
  • Participant will be responsible for cost / organization of their extra day of hotel accommodation and dinner. Costs will not be reimbursed.
  • We will cover coffee and lunch during the bootcamp.



Student Scholarships (two options)

CSDMS

This year CSDMS is offering a limited number of scholarships (up to 12) for graduate students to attend the CSDMS annual meeting. Three scholarships will be offered for the purpose of increasing participation of underrepresented students. To be eligible, graduate students need to meet the following requirements:
  • Attend the whole meeting (May 17-19, 2016)
  • Submit an abstract
  • Be enrolled as a graduate student at the time of the meeting (bring proof)
  • Submit a letter of motivation that states why you wish to participate in the meeting, and explain how your participation would enhance diversity in the field of surface dynamics modeling.
The CSDMS scholarships will cover:
  • Registration costs
  • Travel (air fare ONLY within the United States and local transport)
  • Per diem to help reimburse the cost of meals from 17-19 May 2016 not offered in the conference schedule

SEN

The Sediment Experimentalist Network (SEN) is sponsoring a data-utilization contest for graduate-student and early-career geoscience modelers who feel passionate about advancing science through experimental data sharing and reuse. The top four winners of the data-utilization contest will have all travel and registration costs paid for.
To apply:
  • Please check the box during registration to indicate that you are applying for the SEN travel grant.
  • Send your application materials (proposal, professional biography) to sedimentexp@gmail.com by April 1, 2016.
  • Full instructions for the travel grant application are available here.

Important dates

  • January 15th: Registration opens
  • March 1st: Deadline for student scholarship applications
  • April 1st: Deadline for abstract submission & early registration
  • May 10th: Deadline late registration. Notice additional costs do apply.
  • May 16th: Optional: pre-conference bootcamp
  • May 17-19th: CSDMS annual meeting
  • May 20th: CSDMS Executive and Steering committees meeting (by invitation only)
CSDMS high res weblogo.jpgSEN-logo.jpeg

* The Sediment Experimentalist Network (SEN) integrates the efforts of sediment experimentalists to build a knowledge base for guidance on best practices for data collection and management. The network facilitates cross-institutional collaborative experiments and communicates with the research community about data and metadata guidelines for sediment-based experiments. This effort aims to improve the efficiency and transparency of sedimentary research for field geologists and modelers as well as experimentalists.