Impact of ENSO regimes on developing- and decaying-phase precipitation during rainy season in China
(2017) In Hydrology and Earth System Sciences 21(11). p.5415-5426- Abstract
This study investigated the influence of five El Niño-Southern Oscillation (ENSO) types on rainy-season precipitation in China: central Pacific warming (CPW), eastern Pacific cooling (EPC), eastern Pacific warming (EPW), conventional ENSO and ENSO Modoki. The multi-scale moving t test was applied to determine the onset and withdrawal of rainy season. Results showed that the precipitation anomaly can reach up to 30 % above average precipitation during decaying CPW and EPW phases. Developing EPW could cause decreasing precipitation over large areas in China with 10-30 % lower than average precipitation in most areas. Conventional El Niño in the developing phase had the largest influence on ENSO-related precipitation among developing ENSO... (More)
This study investigated the influence of five El Niño-Southern Oscillation (ENSO) types on rainy-season precipitation in China: central Pacific warming (CPW), eastern Pacific cooling (EPC), eastern Pacific warming (EPW), conventional ENSO and ENSO Modoki. The multi-scale moving t test was applied to determine the onset and withdrawal of rainy season. Results showed that the precipitation anomaly can reach up to 30 % above average precipitation during decaying CPW and EPW phases. Developing EPW could cause decreasing precipitation over large areas in China with 10-30 % lower than average precipitation in most areas. Conventional El Niño in the developing phase had the largest influence on ENSO-related precipitation among developing ENSO and ENSO Modoki regimes. Decaying ENSO also showed a larger effect on precipitation anomalies, compared to decaying ENSO Modoki. The difference between rainy-season precipitation under various ENSO regimes may be attributed to the combined influence of anti-cyclone in the western North Pacific and the Indian monsoon. Stronger monsoon and anti-cyclone are associated with enhanced rainy-season precipitation. The results suggest a certain predictability of rainy-season precipitation related to ENSO regimes.
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- author
- Cao, Qing ; Hao, Zhenchun ; Yuan, Feifei LU ; Su, Zhenkuan ; Berndtsson, Ronny LU ; Hao, Jie and Nyima, Tsring
- organization
- publishing date
- 2017-11-06
- type
- Contribution to journal
- publication status
- published
- subject
- in
- Hydrology and Earth System Sciences
- volume
- 21
- issue
- 11
- pages
- 12 pages
- publisher
- European Geophysical Society
- external identifiers
-
- scopus:85032968779
- wos:000414436100001
- ISSN
- 1027-5606
- DOI
- 10.5194/hess-21-5415-2017
- language
- English
- LU publication?
- yes
- id
- cc34520d-6d3c-48be-b942-0a948fbb55d4
- date added to LUP
- 2017-11-16 07:57:00
- date last changed
- 2025-01-08 00:31:52
@article{cc34520d-6d3c-48be-b942-0a948fbb55d4, abstract = {{<p>This study investigated the influence of five El Niño-Southern Oscillation (ENSO) types on rainy-season precipitation in China: central Pacific warming (CPW), eastern Pacific cooling (EPC), eastern Pacific warming (EPW), conventional ENSO and ENSO Modoki. The multi-scale moving t test was applied to determine the onset and withdrawal of rainy season. Results showed that the precipitation anomaly can reach up to 30 % above average precipitation during decaying CPW and EPW phases. Developing EPW could cause decreasing precipitation over large areas in China with 10-30 % lower than average precipitation in most areas. Conventional El Niño in the developing phase had the largest influence on ENSO-related precipitation among developing ENSO and ENSO Modoki regimes. Decaying ENSO also showed a larger effect on precipitation anomalies, compared to decaying ENSO Modoki. The difference between rainy-season precipitation under various ENSO regimes may be attributed to the combined influence of anti-cyclone in the western North Pacific and the Indian monsoon. Stronger monsoon and anti-cyclone are associated with enhanced rainy-season precipitation. The results suggest a certain predictability of rainy-season precipitation related to ENSO regimes.</p>}}, author = {{Cao, Qing and Hao, Zhenchun and Yuan, Feifei and Su, Zhenkuan and Berndtsson, Ronny and Hao, Jie and Nyima, Tsring}}, issn = {{1027-5606}}, language = {{eng}}, month = {{11}}, number = {{11}}, pages = {{5415--5426}}, publisher = {{European Geophysical Society}}, series = {{Hydrology and Earth System Sciences}}, title = {{Impact of ENSO regimes on developing- and decaying-phase precipitation during rainy season in China}}, url = {{http://dx.doi.org/10.5194/hess-21-5415-2017}}, doi = {{10.5194/hess-21-5415-2017}}, volume = {{21}}, year = {{2017}}, }