Open AccessEstablishing the relationship between the CERES window and total channel measured radiances for conditions involving deep convective clouds at night
Author(s) -
Kratz David P.,
Priestley Kory J.,
Green Richard N.
Publication year - 2002
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.67
H-Index - 298
eISSN - 2156-2202
pISSN - 0148-0227
DOI - 10.1029/2001jd001170
Subject(s) - longwave , shortwave , radiometer , environmental science , remote sensing , radiance , radiative transfer , radiant energy , atmosphere (unit) , nadir , atmospheric radiative transfer codes , meteorology , atmospheric sciences , physics , geology , optics , radiation , satellite , astronomy
Characterizing the stability of the Clouds and the Earth's Radiant Energy System (CERES) instrument is critical to obtaining accurate measurements of the radiative energy budget of the Earth's atmosphere‐surface system. Composed of three broadband radiometers, the CERES instrument measures radiances in the shortwave (>2000 cm −1 ), infrared window (835–1250 cm −1 ), and total regions of the spectrum. Such a choice of radiometers does not allow for a straightforward three channel intercomparison of the CERES measurements. We observed, however, the outgoing infrared spectra of high, cold, optically thick clouds were fairly representative of blackbody emission. This observation suggested a potential relationship between the infrared window radiometer and longwave portion of the total radiometer. Using nighttime measurements made by the CERES instrument aboard the Tropical Rainfall Measuring Mission (TRMM) spacecraft during the first eight months of 1998, we were able to determine a highly correlated relationship between the infrared window and total channel radiances for conditions corresponding to high, cold, optically thick clouds. Comparisons were then made between the measurements and reference line‐by‐line calculations. From these comparisons, a quantified relationship was derived between the total and window channel radiances which could accurately reproduce one set of results from the other. Such a relationship has allowed for the establishment of a three channel intercomparison for the CERES instrument with an accuracy of ∼1% for the case of high, cold, optically thick clouds. An independent relationship based upon the tropical mean is shown to produce results which support the three channel analysis for the deep convective cloud systems.