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A list of all pages that have property "CSDMS meeting abstract figure caption" with value "Fig. 2 Photograph of land cover taken in 31/07/2015.". Since there have been only a few results, also nearby values are displayed.

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    • Annualmeeting:2017 CSDMS meeting-035  + (Figure 1. Aerial imagery of a) Rangiroa<br>Atoll and b) Hikueru Atoll in French Polynesia<br>with varying reef islands (motu) morphology<br>on the c) NW coast and the d) south coast.<br>)
    • Annualmeeting:2017 CSDMS meeting-017  + (Figure 1. Landsat image of the GBMD with physiographic regions active, inactive, and tidal based on geological map of Bangladesh by the Geological Survey of Bangladesh and the USGS (Passalacqua et al., 2013).)
    • 2021 CSDMS meeting-094  + (In this project we analyzed coral atolls&lIn this project we analyzed coral atolls<br>by measuring effective reef width,<br>reef width, motu width, motu length,<br>and reef-motu width. These measurements were<br>binned based on cardinal<br>direction from the atoll centroid. We analyzed<br>these metrics in comparison to<br>directionally-binned wave climate data<br>gathered and analyzed from<br>Wave Watch III virtual buoys.ned wave climate data<br>gathered and analyzed from<br>Wave Watch III virtual buoys.)
    • Annualmeeting:2017 CSDMS meeting-047  + (Model results for the Cedar (left column: Model results for the Cedar (left column: a,d,g,j),<br>Skagit (middle column: b,e,h,k), and North Fork Stillaguamish<br>(right column: c,f,i,l) stratigraphic configurations.<br>A-C show the relative subsurface factor of safety for<br>dry model runs. D-F show groundwater flow fields from VS2Dt<br>simulations. G-I show relative subsurface<br>factor of safety for VS2Dt model runs. J-L show<br>the calculated volume and factor of safety for each potential failure<br>plane modeled in Scoops3D.volume and factor of safety for each potential failure<br>plane modeled in Scoops3D.)
    • Meeting:Abstract 2013 CSDMS meeting-030  + (Modeled characteristic timescale of diffusivity using linear theory over depth with varying (a) deep-water wave height with T =8 s and (b) varying wave period with H0 = 1 m.)
    • Meeting:Abstract 2013 CSDMS meeting-069  + (Output of a RASCAL model of the EvergladesOutput of a RASCAL model of the Everglades ridge and slough landscape. Elevated ridges, colonized by sawgrass, are depicted in red. Flow, which is channeled preferentially through the blue sloughs, runs from top to bottom. Recent catastrophic loss of parallel-drainage sloughs in the Everglades has been attributed to reductions in flow velocities and mean water levels. in flow velocities and mean water levels.)
    • 2023 CSDMS meeting-055  + (Photograph of the epiphyte mat in the Tropical Montane<br>Cloud Forest of Monteverde, Costa RIca.)
    • 2019 CSDMS meeting-102  + (Poster image for Real Time ADCIRC Model Guidance For Decision Support.)
    • Meeting:Abstract 2011 CSDMS meeting-066  + (Simulated landslide geometries and model plastic strain (colors): (a) L = 50 m, (b) L = 100 m, (c) L = 200 m, (d) L = 400 m.)
    • 2018 CSDMS meeting-020  + (This flood simulation is a 2-D LISFLOOD-FP<br>simulation including river flows<br>as well as direct rain on floodplain<br>and a tidal-surge boundary.<br>Whiter tones denote deeper flood waters.)
    • Meeting:Abstract 2011 CSDMS meeting-010  + (Time evolution of the c = 0.1 concentratioTime evolution of the c = 0.1 concentration isosurface for a lock-exchange turbidity current interacting with a Gaussian bump for Re = 2,000. The suspension contains a mixture of two particle sizes, with nondimensional settling velocities equal to u_c = 0.035 and u_f = 0.0035$, and initial mass fractions of 90% and 10%, respectively.ss fractions of 90% and 10%, respectively.)
    • 2020 CSDMS meeting-068  + (Timeslices of HYLANDS model run<br>for the Namche Barwa region after<br>5, 500, 1500 and 2000 model years.)
    • Annualmeeting:2017 CSDMS meeting-113  + (Upper left: time series of bed elevation cUpper left: time series of bed elevation changes, dζ/dt, derived from ADCP measurements of suspended particles concentrations; upper right: power spectrum of dζ/dt with 12 dofs at 95% of statistical confidence (interval given by the vertical line); bottom: continuous wavelet transform of dζ/dt using a Morlet wavelet (Gaussian-modulated wave with a normalized frequency of 6) with black lines surrounding confidence levels (95%). See text for details.idence levels (95%). See text for details.)
    • Meeting:Abstract 2011 CSDMS meeting-007  + (r.landscape_evol.py model results for landscape in Mediterranean Spain)