Contrast of local air-sea relationships between 10-20-day and 30-60-day intraseasonal oscillations during May-September over the South China Sea and western North Pacific
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| 024 | 7 | 0 | |a 10.1007/s00382-015-2549-6 |2 doi |
| 035 | |a (NATIONALLICENCE)springer-10.1007/s00382-015-2549-6 | ||
| 245 | 0 | 0 | |a Contrast of local air-sea relationships between 10-20-day and 30-60-day intraseasonal oscillations during May-September over the South China Sea and western North Pacific |h [Elektronische Daten] |c [Kunhui Ye, Renguang Wu] |
| 520 | 3 | |a Present study compares local air-sea relationship of 10-20-day and 30-60-day intraseasonal oscillations (ISOs) over the South China Sea (SCS) and western North Pacific (WNP) during May through September for the period 1998-2010. It is shown that sea surface temperature (SST) has a larger intraseasonal variance in the North Indian Ocean, the SCS, and subtropical WNP on the 30-60-day time scale, but in tropical WNP on the 10-20-day time scale. The local correlation of SST with rain, surface shortwave radiation (SWR) and latent heat flux (LHF) displays a southwest-northeast tilted structure on the 10-20-day time scale, but a broad west-east pattern with a larger correlation on the 30-60-day time scale. The time of SST leading rain is larger in off-equatorial regions than in near-equatorial regions for both types of ISOs, whereas the time of rain leading SST is larger in near-equatorial regions than in off-equatorial regions. A similar feature is seen for SWR, but an opposite feature for LHF. The atmospheric ISOs induce intraseasonal SST variations through cloud-radiation and wind-evaporation changes. The intraseasonal SST variations feedback on the atmosphere through modulation of atmospheric stability over off-equatorial regions on both timescales. The SST impacts on the atmosphere appear larger on the 30-60-day time scale than on the 10-20-day time scale. The distinct spatial patterns of local air-sea relationship on the two types of ISOs are associated with different spatial structures in both atmospheric ISO-associated SWR and LHF anomalies and SST-induced atmospheric stability anomalies. | |
| 540 | |a Springer-Verlag Berlin Heidelberg, 2015 | ||
| 690 | 7 | |a Air-sea interaction |2 nationallicence | |
| 690 | 7 | |a 10-20-Day oscillation |2 nationallicence | |
| 690 | 7 | |a 30-60-Day oscillation |2 nationallicence | |
| 690 | 7 | |a The South China Sea |2 nationallicence | |
| 690 | 7 | |a Boreal summer |2 nationallicence | |
| 700 | 1 | |a Ye |D Kunhui |u Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Shatin, Hong Kong SAR, China |4 aut | |
| 700 | 1 | |a Wu |D Renguang |u Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Shatin, Hong Kong SAR, China |4 aut | |
| 773 | 0 | |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/11-12(2015-12-01), 3441-3459 |x 0930-7575 |q 45:11-12<3441 |1 2015 |2 45 |o 382 | |
| 856 | 4 | 0 | |u https://doi.org/10.1007/s00382-015-2549-6 |q text/html |z Onlinezugriff via DOI |
| 898 | |a BK010053 |b XK010053 |c XK010000 | ||
| 900 | 7 | |a Metadata rights reserved |b Springer special CC-BY-NC licence |2 nationallicence | |
| 908 | |D 1 |a research-article |2 jats | ||
| 949 | |B NATIONALLICENCE |F NATIONALLICENCE |b NL-springer | ||
| 950 | |B NATIONALLICENCE |P 856 |E 40 |u https://doi.org/10.1007/s00382-015-2549-6 |q text/html |z Onlinezugriff via DOI | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Ye |D Kunhui |u Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Shatin, Hong Kong SAR, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Wu |D Renguang |u Institute of Space and Earth Information Science, The Chinese University of Hong Kong, Shatin, Hong Kong SAR, China |4 aut | ||
| 950 | |B NATIONALLICENCE |P 773 |E 0- |t Climate Dynamics |d Springer Berlin Heidelberg |g 45/11-12(2015-12-01), 3441-3459 |x 0930-7575 |q 45:11-12<3441 |1 2015 |2 45 |o 382 | ||