Results 81 to 90 of about 2,590 (160)

Eastward Propagation of Anomalous Indo–Pacific Walker Circulation During ENSO Transition

Geophysical Research Letters, Volume 53, Issue 9, 16 May 2026.
Abstract By analyzing the zonal mass streamfunction over the equatorial Indo–Pacific region in the period 1979–2024, we found that during the decaying phase of 13 out of 31 El Niño‐Southern Oscillation (ENSO) events, the anomalous Indo–Pacific Walker Circulation (IPWC) propagates steadily eastward across the warm pool. Vertical velocity, precipitation,
Longjun Fan, Tao Lian, Ruikun Hu, Ting Liu, Wendi Wu   +4 more
wiley   +1 more source

Response of the West African Monsoon to the Madden–Julian Oscillation [PDF]

, 2009
Observations show that rainfall over West Africa is influenced by the Madden-Julian Oscillation (MJO). A number of mechanisms have been suggested: 1) forcing by equatorial waves; 2) enhanced monsoon moisture supply; and 3) increased African easterly wave
Lavender, Sally L., Matthews, Adrian J.
core   +1 more source

Maintenance of Moisture Anomalies Across Synoptic and Intraseasonal Timescales Over the Indo‐Pacific Warm Pool

Journal of Geophysical Research: Atmospheres, Volume 131, Issue 9, 16 May 2026.
Abstract Moisture variability plays a fundamental role in regulating tropical precipitation; however, the mechanisms that sustain moisture anomalies across different timescales remain unclear. This study examines how moisture anomalies are regulated over the Indo‐Pacific warm pool using the column‐integrated moist static energy (CMSE) budget.
S. M. Navarro, K. Yasunaga, A. Hamada, K. Ueyoshi   +3 more
wiley   +1 more source

Moisture Origin and Transport for Extreme Precipitation over Indonesia’s New Capital City, Nusantara in August 2021

Atmosphere, 2022
Nusantara, Indonesia’s new capital city, experienced a rare extreme rainfall event on 27–28 August 2021. This heavy rainfall occurred in August, the driest month of the year based on the monthly climatology data, and caused severe flooding and landslides.
Anis Purwaningsih, Sandro W. Lubis, Eddy Hermawan, Dita Fatria Andarini, Teguh Harjana, Dian Nur Ratri, Ainur Ridho, Risyanto, Akas Pinaringan Sujalu   +8 more
doaj   +1 more source

Climate fluctuations of tropical coupled system: The role of ocean dynamics [PDF]

, 2006
The tropical oceans have long been recognized as the most important region for large-scale ocean–atmosphere interactions, giving rise to coupled climate variations on several time scales.
Abram, Aceituno, Alexander, An, An, Anderson, Annamalai, Annamalai, Annamalai, Ashok, Ashok, Ashok, Ashok, Balmaseda, Baquero-Bernal, Barreiro, Battisti, Battisti, Behera, Behera, Behera, Behera, Behera, Behringer, Bjerknes, Black, Black, Blanke, Boccaletti, Bourlès, Bourlès, Boyer, Bratcher, Bryden, Burgers, Cadet, Cai, Cane, Carton, Carton, Carton, Carton, Chambers, Chang, Chang, Chang, Chang, Chang, Chang, Chang, Chang, Chao, Chen, Chen, Chepurin, Chiang, Chiang, Chiang, Chiang, Clark, Clarke, Cobb, Collins, Covey, Csanady, Czaja, Davey, Delecluse, Deser, Deser, Dettinger, Dommenget, Dommenget, Dong, Enfield, Enfield, Enomoto, F. Schott, Fauchereau, Fedorov, Fedorov, Feng, Feng, Fischer, Florenchie, Florenchie, Flügel, Flügel, Flügel, Frankignoul, Fratantoni, Fujiwara, Fukumori, G. Meyers, Galanti, Gammelsrød, Ganachaud, Giannini, Giannini, Giannini, Giese, Graham, Gregg, Gu, Gualdi, Gualdi, Guan, Guan, Guilyardi, Han, Harper, Harrison, Hashizume, Hastenrath, Hastenrath, Hastenrath, Hazeleger, Hazeleger, Held, Hendon, Hermes, Hirst, Hirst, Hirst, Hisard, Hisard, Horel, Hoskins, Hoskins, Huang, Huang, Huang, Huang, Hurrell, Iizuka, Inui, Iskandar, J. Carton, Ji, Jin, Jin, Jin, Jin, Jin, Jochum, Jochum, Johnson, Johnson, Joyce, Jury, Kalnay, Katz, Kawase, Kessler, Kessler, Kessler, Kessler, Kessler, Kim, Kirtman, Kirtman, Kirtman, Kirtman, Kleeman, Kleeman, Kleeman, Klein, Klinger, Klinger, Knutson, Knutson, Koberle, Kushnir, Larkin, Latif, Lau, Lazar, Lee, Li, Li, Lindzen, Liu, Liu, Lorenc, Lu, Luo, Luo, Luo, Luther, Luyten, Luyten, Lysne, Madden, Malanotte-Rizzoli, Mantua, Mantua, Mantua, Marshall, Masson, Masson, Masumoto, Masumoto, McCreary, McPhaden, McPhaden, Meehl, Meehl, Mehta, Meinen, Melice, Mercier, Merle, Mestas-Nunez, Meyers, Meyers, Minobe, Mitchell, Molinari, Moore, Moore, Murtugudde, Murtugudde, Mutai, Namias, Neelin, Neelin, Neelin, Neelin, Nitta, Nonaka, Nonaka, Ogallo, Okajima, Okumura, Okumura, O’Brien, P. Chang, P. Schopf, Pedlosky, Penland, Penland, Penland, Perigaud, Philander, Philander, Philander, Philander, Philander, Picaut, Plumb, Prasad, Qu, Qu, Qu, Qu, Rajagopalan, Rao, Rao, Rao, Rao, Reason, Reid, Reverdin, Reverdin, Rodgers, Rodgers, Rodwell, Roemmich, Ropelewski, Rothstein, Rouault, Ruiz-Barradas, S. K. Behera, S. Shetye, S.-P. Xie, Saji, Saji, Saji, Saravanan, Sardeshmukh, Schiller, Schmitz, Schneider, Schneider, Schneider, Schopf, Schopf, Schopf, Schott, Schott, Schott, Seager, Seager, Sengupta, Sengupta, Servain, Servain, Servain, Servain, Shannon, Shetye, Shinoda, Shinoda, Sikka, Snowden, Solow, Sperber, Sprintall, Sterl, Stramma, Stramma, Stramma, Suarez, Sutton, Suzuki, T. Qu, T. Yamagata, Takaya, Takayabu, Tanimoto, Terray, Terray, Tett, Thompson, Thompson, Timmermann, Timmermann, Tomczak, Tourre, Tozuka, Tozuka, Trenberth, Trenberth, Tziperman, Ueda, Umatani, Urban, Vauclair, Vecchi, Vecchi, Vellinga, Venegas, Vinayachandran, Vinayachandran, Visbeck, Vossepoel, W. S. Kessler, Wagner, Wajsowicz, Wallace, Wallace, Wang, Wang, Wang, Wang, Wang, Wang, Webster, Weisberg, Weisberg, Weisberg, Weisberg, White, Wijffels, Wilson, Wu, Wu, Wyrtki, Xie, Xie, Xie, Xie, Xie, Yamagata, Yamagata, Yang, Yeager, Yeh, Yeh, Yeh, Yoshida, Yu, Yu, Zang, Zebiak, Zhang, Zhang, Zhang, Zhang, Zhang, Zhang, Zubair   +391 more
core   +1 more source

Understanding Interannual Variability of Brahmaputra River Basin Flows Through Bayesian Causal Networks

Earth's Future, Volume 14, Issue 5, May 2026.
Abstract Bayesian Causal Networks (BCNs) are adapted to investigate causal factors of hydroclimate variability in the Brahmaputra River Basin (BRB) during the seasonal and sub‐seasonal periods. This is the longest monsoonal river system in India, prone to frequent severe flooding.
Naman Kishan Rastogi, J. S. Nanditha, Balaji Rajagopalan   +2 more
wiley   +1 more source

Boreal Summer Intraseasonal Oscillation Impact on Western North Pacific Typhoons and Rainfall in Taiwan

Terrestrial, Atmospheric and Oceanic Sciences, 2016
This study discusses the boreal summer intraseasonal oscillation (BSISO) impact on the western North Pacific (WNP) typhoons and the summer rainfall in Taiwan.
Chih-wen Hung, Ho-Jiunn Lin, Pei-ken Kao, Ming-fu Shih, Wei-yi Fong   +4 more
doaj   +1 more source

Mechanism for northward propagation of boreal summer intraseasonal oscillation: Convective momentum transport [PDF]

Geophysical Research Letters, 2010
This study demonstrates that the momentum transport by cumulus convection plays a significant role in the organization and northward propagation of intraseasonal (ISO) convection anomalies over the Indian and western Pacific regions during boreal summer.
In‐Sik Kang, Daehyun Kim, Jong‐Seong Kug   +2 more
openaire   +1 more source

Seasonal Predictions and Their Applications in the Mediterranean Region: Part I—Sources of Predictability and Prediction Skill

International Journal of Climatology, Volume 46, Issue 5, April 2026.
The ability to predict climate fluctuations at seasonal timescales offers significant socio‐economic benefits. However, limited understanding of predictability mechanisms and model errors hinders forecast quality. Recent research has improved forecasting systems and data quality.
Gualdi Silvio, Javier García‐Serrano, Constantin Ardilouze, Silvia Terzago, Veronica Torralba, Wafae Badi, Lauriane Batté, Fatima Driouech, Kristina Fröhlich, Ernesto Rodriguez Camino, Esteban Rodriguez Guisado, Massimiliano Pasqui, Andrea Toreti   +12 more
wiley   +1 more source

Weather types across the Maritime Continent: From the diurnal cycle to interannual variations

Frontiers in Environmental Science, 2015
Six weather types (WTs) are computed across the Maritime Continent during austral summer (September--April) using cluster analysis of unfiltered, daily, low-level winds at 850 hPa, by a k-means algorithm.
Vincent eMoron, Vincent eMoron, Andrew William Robertson, Jian-Hua eQian, Michael eGhil, Michael eGhil   +5 more
doaj   +1 more source