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Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set
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| Zeitschriftentitel: | Geophysical Research Letters |
|---|---|
| Personen und Körperschaften: | , , |
| In: | Geophysical Research Letters, 40, 2013, 2, S. 380-385 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
American Geophysical Union (AGU)
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| Schlagwörter: |
| author_facet |
Gao, Si Chiu, Long S. Shie, Chung‐Lin Gao, Si Chiu, Long S. Shie, Chung‐Lin |
|---|---|
| author |
Gao, Si Chiu, Long S. Shie, Chung‐Lin |
| spellingShingle |
Gao, Si Chiu, Long S. Shie, Chung‐Lin Geophysical Research Letters Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set General Earth and Planetary Sciences Geophysics |
| author_sort |
gao, si |
| spelling |
Gao, Si Chiu, Long S. Shie, Chung‐Lin 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2012gl054620 <jats:p>Trends and variations of Goddard Satellite‐based Surface Turbulent Fluxes (GSSTF) version 2c (GSSTF2c) latent heat flux (LHF) are examined. This version of LHF takes account of the correction in Earth incidence angle. The trend of global mean LHF for GSSTF2c is much reduced relative to GSSTF version 2b Set 1 and Set 2 for the same period 1988–2008. Temporal increase of GSSTF2c LHF in the two decades is 11.0%, in which 3.1%, 5.8%, and 2.1% are attributed to the increase in wind, the increase in sea surface saturated air humidity, and the decrease in near‐surface air humidity, respectively. The first empirical orthogonal function of LHF is a conventional El Niño Southern Oscillation (ENSO) mode. However, the trends in LHF are independent of conventional ENSO phenomena. After removing ENSO signal, the pattern of LHF trends is primarily determined by the pattern of air‐sea humidity difference trends.</jats:p> Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set Geophysical Research Letters |
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| title |
Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_unstemmed |
Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_full |
Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_fullStr |
Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_full_unstemmed |
Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_short |
Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_sort |
trends and variations of ocean surface latent heat flux: results from gsstf2c data set |
| topic |
General Earth and Planetary Sciences Geophysics |
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http://dx.doi.org/10.1029/2012gl054620 |
| publishDate |
2013 |
| physical |
380-385 |
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<jats:p>Trends and variations of Goddard Satellite‐based Surface Turbulent Fluxes (GSSTF) version 2c (GSSTF2c) latent heat flux (LHF) are examined. This version of LHF takes account of the correction in Earth incidence angle. The trend of global mean LHF for GSSTF2c is much reduced relative to GSSTF version 2b Set 1 and Set 2 for the same period 1988–2008. Temporal increase of GSSTF2c LHF in the two decades is 11.0%, in which 3.1%, 5.8%, and 2.1% are attributed to the increase in wind, the increase in sea surface saturated air humidity, and the decrease in near‐surface air humidity, respectively. The first empirical orthogonal function of LHF is a conventional El Niño Southern Oscillation (ENSO) mode. However, the trends in LHF are independent of conventional ENSO phenomena. After removing ENSO signal, the pattern of LHF trends is primarily determined by the pattern of air‐sea humidity difference trends.</jats:p> |
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| author | Gao, Si, Chiu, Long S., Shie, Chung‐Lin |
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| description | <jats:p>Trends and variations of Goddard Satellite‐based Surface Turbulent Fluxes (GSSTF) version 2c (GSSTF2c) latent heat flux (LHF) are examined. This version of LHF takes account of the correction in Earth incidence angle. The trend of global mean LHF for GSSTF2c is much reduced relative to GSSTF version 2b Set 1 and Set 2 for the same period 1988–2008. Temporal increase of GSSTF2c LHF in the two decades is 11.0%, in which 3.1%, 5.8%, and 2.1% are attributed to the increase in wind, the increase in sea surface saturated air humidity, and the decrease in near‐surface air humidity, respectively. The first empirical orthogonal function of LHF is a conventional El Niño Southern Oscillation (ENSO) mode. However, the trends in LHF are independent of conventional ENSO phenomena. After removing ENSO signal, the pattern of LHF trends is primarily determined by the pattern of air‐sea humidity difference trends.</jats:p> |
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| physical | 380-385 |
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| spelling | Gao, Si Chiu, Long S. Shie, Chung‐Lin 0094-8276 1944-8007 American Geophysical Union (AGU) General Earth and Planetary Sciences Geophysics http://dx.doi.org/10.1029/2012gl054620 <jats:p>Trends and variations of Goddard Satellite‐based Surface Turbulent Fluxes (GSSTF) version 2c (GSSTF2c) latent heat flux (LHF) are examined. This version of LHF takes account of the correction in Earth incidence angle. The trend of global mean LHF for GSSTF2c is much reduced relative to GSSTF version 2b Set 1 and Set 2 for the same period 1988–2008. Temporal increase of GSSTF2c LHF in the two decades is 11.0%, in which 3.1%, 5.8%, and 2.1% are attributed to the increase in wind, the increase in sea surface saturated air humidity, and the decrease in near‐surface air humidity, respectively. The first empirical orthogonal function of LHF is a conventional El Niño Southern Oscillation (ENSO) mode. However, the trends in LHF are independent of conventional ENSO phenomena. After removing ENSO signal, the pattern of LHF trends is primarily determined by the pattern of air‐sea humidity difference trends.</jats:p> Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set Geophysical Research Letters |
| spellingShingle | Gao, Si, Chiu, Long S., Shie, Chung‐Lin, Geophysical Research Letters, Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set, General Earth and Planetary Sciences, Geophysics |
| title | Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_full | Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_fullStr | Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_full_unstemmed | Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_short | Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| title_sort | trends and variations of ocean surface latent heat flux: results from gsstf2c data set |
| title_unstemmed | Trends and variations of ocean surface latent heat flux: Results from GSSTF2c data set |
| topic | General Earth and Planetary Sciences, Geophysics |
| url | http://dx.doi.org/10.1029/2012gl054620 |