Assessment of NASA GISS CMIP5 and Post-CMIP5 Simulated Clouds and TOA Radiation Budgets Using Satellite Observations. Part II: TOA Radiation Budget and CREsSource: Journal of Climate:;2014:;volume( 028 ):;issue: 005::page 1842Author:Stanfield, Ryan E.
,
Dong, Xiquan
,
Xi, Baike
,
Del Genio, Anthony D.
,
Minnis, Patrick
,
Doelling, David
,
Loeb, Norman
DOI: 10.1175/JCLI-D-14-00249.1Publisher: American Meteorological Society
Abstract: n Part I of this study, the NASA GISS Coupled Model Intercomparison Project (CMIP5) and post-CMIP5 (herein called C5 and P5, respectively) simulated cloud properties were assessed utilizing multiple satellite observations, with a particular focus on the southern midlatitudes (SMLs). This study applies the knowledge gained from Part I of this series to evaluate the modeled TOA radiation budgets and cloud radiative effects (CREs) globally using CERES EBAF (CE) satellite observations and the impact of regional cloud properties and water vapor on the TOA radiation budgets. Comparisons revealed that the P5- and C5-simulated global means of clear-sky and all-sky outgoing longwave radiation (OLR) match well with CE observations, while biases are observed regionally. Negative biases are found in both P5- and C5-simulated clear-sky OLR. P5-simulated all-sky albedo slightly increased over the SMLs due to the increase in low-level cloud fraction from the new planetary boundary layer (PBL) scheme. Shortwave, longwave, and net CRE are quantitatively analyzed as well. Regions of strong large-scale atmospheric upwelling/downwelling motion are also defined to compare regional differences across multiple cloud and radiative variables. In general, the P5 and C5 simulations agree with the observations better over the downwelling regime than over the upwelling regime. Comparing the results herein with the cloud property comparisons presented in Part I, the modeled TOA radiation budgets and CREs agree well with the CE observations. These results, combined with results in Part I, have quantitatively estimated how much improvement is found in the P5-simulated cloud and radiative properties, particularly over the SMLs and tropics, due to the implementation of the new PBL and convection schemes.
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| contributor author | Stanfield, Ryan E. | |
| contributor author | Dong, Xiquan | |
| contributor author | Xi, Baike | |
| contributor author | Del Genio, Anthony D. | |
| contributor author | Minnis, Patrick | |
| contributor author | Doelling, David | |
| contributor author | Loeb, Norman | |
| date accessioned | 2017-06-09T17:10:24Z | |
| date available | 2017-06-09T17:10:24Z | |
| date copyright | 2015/03/01 | |
| date issued | 2014 | |
| identifier issn | 0894-8755 | |
| identifier other | ams-80551.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4223455 | |
| description abstract | n Part I of this study, the NASA GISS Coupled Model Intercomparison Project (CMIP5) and post-CMIP5 (herein called C5 and P5, respectively) simulated cloud properties were assessed utilizing multiple satellite observations, with a particular focus on the southern midlatitudes (SMLs). This study applies the knowledge gained from Part I of this series to evaluate the modeled TOA radiation budgets and cloud radiative effects (CREs) globally using CERES EBAF (CE) satellite observations and the impact of regional cloud properties and water vapor on the TOA radiation budgets. Comparisons revealed that the P5- and C5-simulated global means of clear-sky and all-sky outgoing longwave radiation (OLR) match well with CE observations, while biases are observed regionally. Negative biases are found in both P5- and C5-simulated clear-sky OLR. P5-simulated all-sky albedo slightly increased over the SMLs due to the increase in low-level cloud fraction from the new planetary boundary layer (PBL) scheme. Shortwave, longwave, and net CRE are quantitatively analyzed as well. Regions of strong large-scale atmospheric upwelling/downwelling motion are also defined to compare regional differences across multiple cloud and radiative variables. In general, the P5 and C5 simulations agree with the observations better over the downwelling regime than over the upwelling regime. Comparing the results herein with the cloud property comparisons presented in Part I, the modeled TOA radiation budgets and CREs agree well with the CE observations. These results, combined with results in Part I, have quantitatively estimated how much improvement is found in the P5-simulated cloud and radiative properties, particularly over the SMLs and tropics, due to the implementation of the new PBL and convection schemes. | |
| publisher | American Meteorological Society | |
| title | Assessment of NASA GISS CMIP5 and Post-CMIP5 Simulated Clouds and TOA Radiation Budgets Using Satellite Observations. Part II: TOA Radiation Budget and CREs | |
| type | Journal Paper | |
| journal volume | 28 | |
| journal issue | 5 | |
| journal title | Journal of Climate | |
| identifier doi | 10.1175/JCLI-D-14-00249.1 | |
| journal fristpage | 1842 | |
| journal lastpage | 1864 | |
| tree | Journal of Climate:;2014:;volume( 028 ):;issue: 005 | |
| contenttype | Fulltext |