Earth system models (ESMs), used in climate simulations and projections, typically use grids of 50–200 km resolution. These are considered relatively coarse with limited ability to resolve land surface variability. Earth system models (ESMs), used in climate simulations and projections, typically use grids of 50–200 km resolution. These are considered relatively coarse with limited ability to resolve land surface variability. Earth Sciences Environment Phys.org – latest science and technology news stories
Capturing finer-scale topographic differences improves Earth system model capability to reproduce observations
