Results 61 to 70 of about 2,670 (210)

The intraseasonal oscillation of pCO2 over the southeast coast of Vietnam in boreal summer

Environmental Research Communications
The intraseasonal oscillation (ISO) of the oceanic surface partial pressure of carbon dioxide ( p CO _2 ) is one of the primary subsequent effects of the monsoon-driven upwelling along the southeast coast of Vietnam (SCV) in boreal summer.
Miaoyin Zhang, Xueming Zhu, Xuanliang Ji
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
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Impact of Arctic sea ice on the boreal summer intraseasonal oscillation

Climate Dynamics
AbstractThis study investigates the relationship between sea ice concentration (SIC) in the Arctic Ocean and the Boreal Summer Intraseasonal Oscillation (BSISO) from 1991 to 2020 and its underlying mechanism. A significantly positive (negative) correlation was found between the frequency of phase 7 (3) of BSISO1 (30–60 d) and the preceding winter SIC ...
Zihuang Xie, Yao Ha, Yimin Zhu, Yijia Hu, Zhong Zhong   +4 more
openaire   +1 more source

Interannual Variations of the Boreal Summer Intraseasonal Oscillation in the Asian–Pacific Region* [PDF]

Journal of Climate, 2003
Abstract A finite-domain wavenumber–frequency analysis was proposed to objectively measure the interannual variability of the boreal summer intraseasonal oscillation (ISO) in the Asian–Pacific region. The strongest interannual variations of the ISO are found in the off-equatorial western North Pacific (WNP).
Haiyan Teng, Bin Wang
openaire   +1 more source

Impact on Extreme Rainfall and Flood Events during Boreal Summer Intraseasonal Oscillation (BSISO) in Aceh Province, Indonesia

JGEET: Journal of Geoscience, Engineering, Environment and Technology
The Boreal Summer Intraseasonal Oscillation (BSISO) is intraseasonal climate variability in addition to the Madden-Julian Oscillation (MJO) that affects weather and climate in the Indo-Pacific region including the Province of Aceh. The impact of BSISO on
Harisa Bilhaqqi Qalbi, Faisal Abdullah, Nazli Ismail   +2 more
doaj   +1 more source

Subseasonal processes of triple extreme heatwaves over the Yangtze River Valley in 2022

Weather and Climate Extremes, 2023
Historical extreme heatwaves struck the Yangtze River Valley (YRV) in the boreal summer of 2022, severely impacting agricultural production, electricity supply, and resident health in China.
Boqi Liu, Congwen Zhu, Shuangmei Ma, Yuhan Yan, Ning Jiang   +4 more
doaj   +1 more source

The surface diurnal warm layer in the Indian Ocean during CINDY/DYNAMO [PDF]

, 2014
A surface diurnal warm layer is diagnosed from Seaglider observations, and develops on half the days in the CINDY/DYNAMO Indian Ocean experiment. The diurnal warm layer occurs on days of high solar radiation flux (>80 W m-2) and low wind speed (
Baranowski, Dariusz, Flatau, Piotr, Heywood, Karen, Matthews, Adrian, Schmidtko, Sunke   +4 more
core   +1 more source

Interannual variability of the onset of the South China Sea summer monsoon [PDF]

, 2015
This article investigates the year-to-year variability of the onset of the South China Sea summer monsoon (SCSSM) and the possible influences exerted by the surface temperature anomalies over land and sea. Early and late monsoon onsets are related to the
Adler, Ashok, Bellon, Chen, Ding, Ding, Ding, Ding, Feng, Feng, Feng, Gao, Graf, Huang, Jiang, Kajikawa, Kajikawa, Kajikawa, Kalnay, Kueh, Kug, Larkin, Larkin, Lau, Lee, Li, Li, Liang, Liebmann, Lin, Liu, Liu, Lu, Ohba, Okumura, Okumura, Qian, Tanaka, Tanaka, Tao, Taschetto, Wang, Wang, Wang, Wang, Wang, Wang, Weng, Wu, Wu, Wu, Wu, Wu, Wu, Yan, Yang, Yeh, Yu, Yuan, Yuan, Zhang, Zhang, Zhang, Zhou, Zhou, Zhou, Zhu   +66 more
core   +2 more sources

Real-time extraction of the Madden-Julian oscillation using empirical mode decomposition and statistical forecasting with a VARMA model [PDF]

, 2008
A simple guide to the new technique of empirical mode decomposition (EMD) in a meteorological-climate forecasting context is presented. A single application of EMD to a time series essentially acts as a local high-pass filter.
Adrian J. Matthews, Ansley, Barnaby S. Love, Box, Coughlin, Duffy, Ferranti, Gareth J. Janacek, Gill, Goswami, Hall, Hendon, Hendon, Huang, Huang, Jones, Jones, Li, Liebmann, Lo, Madden, Maharaj, Maloney, Matthews, Mo, Salby, Shea, Waliser, Waliser, Waliser, Waliser, Wheeler, Wheeler, Wheeler, Woolnough, Wu, Zhang   +36 more
core   +1 more source

The Boreal-Summer Intraseasonal Oscillations Simulated in a Hybrid Coupled Atmosphere–Ocean Model* [PDF]

Monthly Weather Review, 2004
Abstract The boreal-summer intraseasonal oscillation (BSISO) simulated by an atmosphere–ocean coupled model is validated with the long-term observations [Climate Prediction Center (CPC) Merged Analysis of Precipitation (CMAP) rainfall, ECMWF analysis, and Reynolds' SST].
Bin Wang, Xiouhua Fu
openaire   +1 more source