Vol. 29, issue 07, article # 13

Abstract:

The paper presents a principal component (PC) method for solution of the inverse problem of retrieval of HDO to H₂O ratio in the atmosphere from spectra of outgoing Earth’s heat radiation measured with high resolution Fourier spectrometers from satellites. The method is tested by using IMG/ADEOS spectrum data over target area of Pacific Ocean. Intercomparison of results of retrieval of latitudinal distribution of HDO to H₂O ratio in the atmosphere from the IMG spectrum data using PC method with the results obtained from TES/AURA spectrum data using conventional optimal estimation methodology is presented. Good agreement between the data in Northern hemisphere and some discrepancies in Southern hemisphere are discussed.

Keywords:

atmosphere, satellite sounding, water vapour isotopologues

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