dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Evaluation of ECHAM5-HAM simulated Surface, TOA and Atmospheric Radiation Budgets using Global CERES-BSRN Observations
VerfasserIn Xiquan Dong, Baike Xi, Martin Wild, Doris Folini, Minnis Minnis, Norman Loeb
Konferenz EGU General Assembly 2010
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 12 (2010)
Datensatznummer 250034034
 
Zusammenfassung
Atmospheric column absorption of solar radiation (Acol) is a fundamental part of the Earth’s energy cycle but is an extremely difficult quantity to measure directly. To investigate Acol, we have collocated satellite-surface observations over the 35 selected BSRN surface sites during the period March 2000-December 2004. The surface radiation budgets are averaged from the BSRN Shortwave (SW) observations over a 1-hour interval centered at the time of the NASA Terra and Aqua satellites overpass, and the TOA radiation budgets are averaged from the closest FOV satellite data to the BSRN stations. Then the atmospheric column SW absorption was inferred from the satellite TOA albedo and BSRN surface absorption. Monthly means of Acol, TOA albedo, and surface absorption are calculated under both clear- and all-sky conditions over the 35 selected BSRN sites which have covered different climate regimes. To evaluate the GCM simulations, we have collected the ECHAM5-HAM simulated surface, TOA and atmospheric radiation budgets by researchers at ETH Zurich and compared those simulations with observations. The preliminary comparisons have shown that the ECHAN5 simulated clear-sky surface absorption, TOA albedo, and Acol agree very well (1-3%) with observations. Under all-sky conditions, they have strong correlations with CERES-derived cloud fraction. The simulated surface absorption is lower and TOA albedo is higher than those under clear skies, but ACOL does not increase too much. However, there are relatively large differences over some regions and months. A further study is needed.