East asian subtropical jet
WebThis study aimed to identify the patterns and location of the jet stream in. Jet streams are atmospheric phenomena that operate on a synoptic scale and can intensify the descending/ascending conditions of the air at the lower levels of the atmosphere. This study aimed to identify the patterns and location of the jet stream in WebJan 16, 2024 · The EASJ is a narrow and strong westerly belt over subtropical East Asia, which is tied to teleconnections affecting the weather and climate in Asia, the North …
East asian subtropical jet
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WebApr 1, 2024 · The East Asian subtropical westerly jet (EASWJ), an important component of the summer monsoon circulations, was investigated to elucidate the dynamical linkages between its intraseasonal...
WebUsing the National Center for Environment Prediction Climate Forecast System Reanalysis coupled dataset during 1979-2010, we selected four subseasonal indexes from the 16 East Asian Summer... WebHere we identify an association between the East Asian Subtropical Jet Stream (EASJ) during July-October and the frequency of Atlantic TCs (wind speed >= 34 knot) and …
WebSep 1, 2014 · According to the observational data analyses, the East Asian jet system consists of two separate branches: the East Asian subtropical jet (EASJ) and the East Asian polar front jet (EAPJ). The EASJ is strong and steady, while the EAPJ has significant transient characteristics ( Lee and Kim 2003 ). WebApr 10, 2024 · The East Asian summer monsoon (EASM) is a unique regional monsoon in the extratropics involving not only tropical but midlatitude processes. Most of the previous studies identified the role of condensational heating which is largely relevant to the tropical moisture transport in determining the dynamical structure of EASM.
WebJun 6, 2016 · In the cold season, two jets are located at the southern and northern flanks of the Tibetan Plateau (TP), namely, the East Asian subtropical jet (EASJ) and East Asian polar-front jet (EAPJ, also known as East Asian eddy-driven jet), respectively.
WebJul 12, 2013 · Previous studies (Yu et al. 2004; Yu et al. 2008) found that in the last 20 years, the further south position of the East Asian subtropical westerly jet was well related to the summer upper troposphere cooling over eastern Asia, and resulted in weakening East Asian summer monsoon and more rainfall over the Yangtze River basin. dewberry hallWebAug 24, 2024 · Many works have studied the relationship between the East Asian subtropical westerly jet (EASWJ) and East Asian summer monsoon (EASM) from different perspectives, such as the meridional displacement of the EASWJ and the seasonal transition [ 3 ], the onset of the EASM [ 4, 5] and Meiyu in East Asia [ 6 ], and the north … church of st sophia ohridWebJul 8, 2024 · Here we identify an association between the East Asian Subtropical Jet Stream (EASJ) during July–October and the frequency of Atlantic TCs (wind speed ≥34 knot) and hurricanes (wind speed ≥64 knot) during August–November based on observations for 1980–2024. church of st stephen portugalWebNov 9, 2024 · The leading inter-model spread in winter surface air temperature over the Eurasian continent is a cold pattern from the CMIP6 models The weakened-East Asian polar front jet-enhanced-East Asian subtropical jet variation would result in this inter-model spread due to the strengthened East Asian winter monsoon dewberry group atlanta gaWebJan 23, 2024 · As shown in Figure 6g, East Asian subtropical jet (EASJ) shows a southward shift with the corresponding vertical motion change in urbanization experiment of positive PDO phase which induces a decrease in precipitation over 30–40° N of China, while there is no obvious change of EASJ position in urbanization experiment of negative PDO … church of st stephen walbrookWebMar 3, 2024 · Temperature changes in different latitudes reduced vertical wind shear and therefore weakened the summertime Eurasian subtropical westerly jet -- the ribbon of wind which extends east over... dewberry group incWebApr 30, 2024 · The in-phase configuration of the WNPSH and EAJ is characterized by the westward (eastward) extension of the WNPSH and the southward (northward) shift of the EAJ, which is consistent with the general correspondence between their variations. The out-of-phase configuration includes the residual cases. dewberry group charleston