Drilldown: BibEntryCargo

From CSDMS
BibEntryCargo > Journal: Geoscientific Model Development & Note: Auto downloaded ref at: 2019-12-31

Use the filters below to narrow your results.

Title:
ATAT 1.1, the Automated Timing Accordance Tool for comparing ice-sheet model output with geochronological data (1) · EwE-F 1.0: an implementation of Ecopath with Ecosim in Fortran 95/2003 for coupling and integration with other models (1) · ISSM-SESAW v1.0: mesh-based computation of gravitationally consistent sea-level and geodetic signatures caused by cryosphere and climate driven mass change (1) · Improved routines to model the ocean carbonate system: mocsy 2.0 (1) · Open-source modular solutions for flexural isostasy: gFlex v1.0 (1) · Optimal numerical solvers for transient simulations of ice flow using the Ice Sheet System Model (ISSM versions 4.2.5 and 4.11) (1) · Quantitative stratigraphic analysis in a source-to-sink numerical framework (1) · Regional climate hindcast simulations within EURO-CORDEX: evaluation of a WRF multi-physics ensemble (1) · Simulating the thermal regime and thaw processes of ice-rich permafrost ground with the land-surface model CryoGrid 3 (1) · Terrainbento 1.0: a Python package for multi-model analysis in long-term drainage basin evolution (1) · The Landlab v1.0 OverlandFlow component: a Python tool for computing shallow-water flow across watersheds (1) · The North American Carbon Program Multi-scale Synthesis and Terrestrial Model Intercomparison Project – Part 2: Environmental driver data (1) · The SPACE 1.0 model: a Landlab component for 2-D calculation of sediment transport, bedrock erosion, and landscape evolution (1) · eSCAPE: Regional to Global Scale Landscape Evolution Model v2.0 (1)
Editors:
Journal: (Click arrow to add another value)
Booktitle:
Volume:
10 (3) · 12 (4) · 7 (1) · 8 (3) · 9 (3)
ISBN:
Note: (Click arrow to add another value)

Showing below up to 14 results in range #1 to #14.

View (previous 250 | next 250) (20 | 50 | 100 | 250 | 500)


View (previous 250 | next 250) (20 | 50 | 100 | 250 | 500)