Global eastward propagation signals associated with the 4-5-year ENSO cycle
| LEADER | caa a22 4500 | ||
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| 001 | 605475016 | ||
| 003 | CHVBK | ||
| 005 | 20210128100350.0 | ||
| 007 | cr unu---uuuuu | ||
| 008 | 210128e20150501xx s 000 0 eng | ||
| 024 | 7 | 0 | |a 10.1007/s00382-014-2422-z |2 doi |
| 035 | |a (NATIONALLICENCE)springer-10.1007/s00382-014-2422-z | ||
| 245 | 0 | 0 | |a Global eastward propagation signals associated with the 4-5-year ENSO cycle |h [Elektronische Daten] |c [S.-Y. Simon Wang, Xianan Jiang, Boniface Fosu] |
| 520 | 3 | |a Longitude-time evolution of sea surface temperature anomalies (SSTA) reveals a slow southeastward propagation from the western North Pacific (WNP) around 20°N to the Niño-3.4 region in the equatorial Central Pacific. The propagation is manifested as a narrow, southwest-northeast oriented SSTA band across the subtropical North Pacific, and its journey takes about 2-3years. The propagating SSTA appears to engage the initiation of the El Niño-Southern Oscillation (ENSO). The anomalies of surface winds, sea level pressure, outgoing longwave radiation, and velocity potential all exhibit a concurrent and distinct eastward propagation, one that appears to be circumglobaland is coupled with the predominant 4-5year frequency of the ENSO cycle. It is suggested that the previously found warming/cooling in the Indian Ocean induced by El Niño/La Niña, the progressive SSTA and wind anomalies across the Indian Ocean towards the WNP, and the predominant 4-5-year frequency of the North Pacific Oscillation collectively contribute to the reported SSTA propagation . The findings implicate that monitoring the SSTA propagation from the WNP towards the tropical central Pacific could be useful in tracking the ENSO development. | |
| 540 | |a Springer-Verlag Berlin Heidelberg, 2014 | ||
| 690 | 7 | |a ENSO cycle |2 nationallicence | |
| 690 | 7 | |a SST propagation |2 nationallicence | |
| 690 | 7 | |a Precursor |2 nationallicence | |
| 690 | 7 | |a Prediction |2 nationallicence | |
| 690 | 7 | |a WNP |2 nationallicence | |
| 700 | 1 | |a Simon Wang |D S.-Y |u Utah Climate Center, Utah State University, Logan, UT, USA |4 aut | |
| 700 | 1 | |a Jiang |D Xianan |u Joint Institute for Regional Earth System Science and Engineering, UCLA, Los Angeles, CA, USA |4 aut | |
| 700 | 1 | |a Fosu |D Boniface |u Climate Sciences Program, Utah State University, Logan, UT, USA |4 aut | |
| 773 | 0 | |t Climate Dynamics |d Springer Berlin Heidelberg |g 44/9-10(2015-05-01), 2825-2837 |x 0930-7575 |q 44:9-10<2825 |1 2015 |2 44 |o 382 | |
| 856 | 4 | 0 | |u https://doi.org/10.1007/s00382-014-2422-z |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/s00382-014-2422-z |q text/html |z Onlinezugriff via DOI | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Simon Wang |D S.-Y |u Utah Climate Center, Utah State University, Logan, UT, USA |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Jiang |D Xianan |u Joint Institute for Regional Earth System Science and Engineering, UCLA, Los Angeles, CA, USA |4 aut | ||
| 950 | |B NATIONALLICENCE |P 700 |E 1- |a Fosu |D Boniface |u Climate Sciences Program, Utah State University, Logan, UT, USA |4 aut | ||
| 950 | |B NATIONALLICENCE |P 773 |E 0- |t Climate Dynamics |d Springer Berlin Heidelberg |g 44/9-10(2015-05-01), 2825-2837 |x 0930-7575 |q 44:9-10<2825 |1 2015 |2 44 |o 382 | ||