Access to these data is available to any registered CEDA user. The SO2 injection matrix simulations were performed to perform a system identification of the Whole Atmosphere Community Climate Model WACCM , to identify the aerosol optical depth and climate response of stratospheric SO2 injections for different locations and amount. Sea Water Salinity so [1. Strain Rate Divergence of Sea Ice divice [s-1]. Temperature of Soil tsl [K]. No news update for this record.
| Uploader: | Zulukus |
| Date Added: | 26 July 2004 |
| File Size: | 40.38 Mb |
| Operating Systems: | Windows NT/2000/XP/2003/2003/7/8/10 MacOS 10/X |
| Downloads: | 24558 |
| Price: | Free* [*Free Regsitration Required] |
All data are from uncoupled CLM or CLM-CAM simulations, and were run in one of four cover crop configurations that modified the cropland area during the fallow season over North America in the land surface data set used within each simulation: Snow Area Fraction names: Evaporation from Canopy evspsblveg [kg m-2 s-1]. Condensed Water Path clwvi [kg m-2].
Dataset: CCSM4/CESM Model Output
Carbon Mass Flux into Atmosphere due to Heterot Carbon Mass in Fast Soil Pool names: Southern Ocean Eddies simulations. Global monthly-mean history files used for the analysis presented in Schmidt et al. The first simulations of stratospheric sulfate aerosol geoengineering using multiple injection locations to cmi5p multiple simultaneous surface temperature objectives.
Total Soil Moisture Content mrso [kg m-2]. Described in the manuscript: Global Mean Sea Water Salinity soga [1].
Carbon Mass Flux into Atmosphere due to Growth By continuing to use this website you are agreeing to our use of cookies. Upward Ocean Mass Transport wmo [kg s-1]. Surface Downward Sensible Heat Flux names: Temperature of Soil tsl [K].
No related previous identifiers. These are historical simulations. Carbon Mass Flux out of Atmosphere due to Gross Liquid Water Content of Snow Layer lwsnl [kg m-2].
CESM Experiments
Carbon Mass in Soil Pool units: Capacity of Soil to Store Water names: These are the control simulations; the geoengineering feedback simulations are linked below.
Surface Upwelling Longwave Radiation rlus dara m-2]. Surface Snow Amount snw [kg m-2]. Mass Fraction of Cloud Liquid Water clw [1].
Air Temperature tas [K]. Convective Precipitation prc [kg m-2 s-1]. Convective Mass Flux names: Compressive Sea Ice Strength streng [N m-1].
See linked documentation for available information for each component. Geoengineering Large Ensemble Historical.
profkingtrebal.gq
SandersonThe importance of aerosol scenarios in projections of future heat extremes, Climatic Change, 1—14, doi: The model has a horizontal resolution of 1. Snow Soot Content sootsn [kg m-2].
Carbon Mass in Litter Pool cLitter [kg m-2].
No comments:
Post a Comment