Member Since 1993
Charlie S. Zender
Professor, University of California Irvine
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Climate Sensitivity to Improved Spectral Solar Insolation in E3SM
AGU 2024
atmospheric sciences | 12 december 2024
Juan Tolento, Charles S. Zender, Andrew Roberts, E...
Surface and atmospheric radiative processes depend strongly on wavelength. For example, snow albedo shifts from highly reflective at wavelengths <0...
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The Climate & Forecast (CF) Metadata Convention for Quantization
AGU 2024
informatics | 11 december 2024
Charles S. Zender
An increasingly important and easy way to tame the geophysical data deluge is to quantize the random or unwanted trailing bits of IEEE floating point ...
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Surface and Atmospheric Heating Responses to Spectrally Resolved Albedo of Frozen and Liquid Water Surfaces
AGU 2024
cryosphere | 11 december 2024
Juan Tolento, Charles S. Zender, Chloe Whicker Cla...
Multiple Earth system models (ESMs) discretize surface albedo into two semi-broadbands comprising the UV/visible (VIS) and near-infrared (NIR) wavelen...
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Development and Testing of a Coupled Greenland Ice Sheet Component in E3SM
AGU 2024
global environmental change | 09 december 2024
Stephen F. Price, Carolyn B. Begeman, Darin Comeau...
We report on efforts to couple, validate, and apply a dynamic Greenland Ice Sheet (GIS) component within DOEs Energy Exascale Earth System Model (E3SM...
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Analyzing Surface Mass Balance from E3SM Against RACMO and Observational Data
AGU 2024
cryosphere | 09 december 2024
Chloe Whicker Clarke, Charles S. Zender, Michael K...
It is increasingly important to accurately simulate the Greenland Ice Sheet (GrIS) surface mass balance (SMB) and surface energy budget (SEB) as the G...
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Surface and Atmospheric Heating Responses to Spectrally Resolved Albedo of Frozen and Liquid Water Surfaces
JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES
27 april 2024
Juan Tolento, Charles S. Zender, Chloe Whicker Cla...

Multiple Earth system models (ESMs) discretize surface albedo into two semi‐broadbands comprising the UV/visible and near‐infrared (NIR...

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The Effect of Physically Based Ice Radiative Processes on Greenland Ice Sheet Albedo and Surface Mass Balance in E3SM
JOURNAL OF GEOPHYSICAL RESEARCH: ATMOSPHERES
08 april 2024
Chloe Whicker Clarke, Raf Antwerpen, Mark Flanner,...

A significant portion of surface melt on the Greenland Ice Sheet (GrIS) is due to dark ice regions in the ablation zone, where solar absorption is ...

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Realistic representation of bare-ice albedo: Effects on Greenland surface mass balance in the Energy Exascale Earth System Model (E3SM)
SNOW AND FIRN PROCESSES ON GLACIERS AND ICE SHEETS I POSTER
cryosphere | 14 december 2023
Chloe Whicker Clarke, Raf Antwerpen, Mark Flanner,...
Surface melt from the Greenland Ice Sheet (GrIS) is a large contributor to sea level rise. Melt on the surface of the ice sheet is partially controlle...
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