Show simple item record

dc.contributor.authorSomeya, Y.
dc.contributor.authorYoshida, Y.
dc.contributor.authorOhyama, H.
dc.contributor.authorNomura, S.
dc.contributor.authorKamei, A.
dc.contributor.authorMorino, I.
dc.contributor.authorMukai, H.
dc.contributor.authorMatsunaga, T.
dc.contributor.authorLaughner, J.L.
dc.contributor.authorVelazco, V.A.
dc.contributor.authorHerkommer, B.
dc.contributor.authorTé, Y.
dc.contributor.authorSha, M.K.
dc.contributor.authorKivi, R.
dc.contributor.authorZhou, M.
dc.contributor.authorOh, Y.S.
dc.contributor.authorDeutscher, N.M.
dc.contributor.authorGriffith, D.W.T.
dc.date2023
dc.date.accessioned2023-03-22T13:11:24Z
dc.date.available2023-03-22T13:11:24Z
dc.identifier.urihttps://orfeo.belnet.be/handle/internal/10829
dc.descriptionThe National Institute for Environmental Studies has provided the column-averaged dry-air mole fraction of carbon dioxide and methane (XCO2 and XCH4) products (L2 products) obtained from the Greenhouse gases Observing SATellite (GOSAT) for more than a decade. Recently, we updated the retrieval algorithm used to produce the new L2 product, V03.00. The main changes from the previous version (V02) of the retrieval algorithm are the treatment of cirrus clouds, the degradation model of the Thermal And Near-infrared Spectrometer for carbon Observation–Fourier Transform Spectrometer (TANSO–FTS), solar irradiance spectra, and gas absorption coefficient tables. The retrieval results from the updated algorithm showed improvements in fitting accuracies in the O2 A, weak CO2, and CH4 bands of TANSO–FTS, although the residuals increase in the strong CO2 band over the ocean. The direct comparison of the new product obtained from the updated (V03) algorithm with the previous version V02.90/91 and the validations using the Total Carbon Column Observing Network revealed that the V03 algorithm increases the amount of data without diminishing the data qualities of XCO2 and XCH4 over land. However, the negative bias of XCO2 is larger than that of the previous version over the ocean, and bias correction is still necessary. Additionally, the V03 algorithm resolves the underestimation of the XCO2 growth rate compared with the in situ measurements over the ocean recently found using V02.90/91 and V02.95/96.
dc.languageeng
dc.titleUpdate on the GOSAT TANSO–FTS SWIR Level 2 retrieval algorithm
dc.typeArticle
dc.subject.frascatiEarth and related Environmental sciences
dc.audienceScientific
dc.source.titleAtmospheric Measurement Techniques
dc.source.volume16
dc.source.issue6
dc.source.page1477-1501
Orfeo.peerreviewedYes
dc.identifier.doi10.5194/amt-16-1477-2023
dc.identifier.scopus


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record