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Journal of Meteorological Research 2015年第4期29卷 562-575页

作者：何超周天军吴波 Institute of Tropical and Marine Meteorology China Meteorological Administration State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics Institute of Atmospheric Physics Chinese Academy of Sciences Joint Center for Global Change Studies

The western north pacific subtropical high （WNPSH） is an important circulation system that impacts the East Asian summer climate. The interannual variability of the WNPSH is modulated by tropical air-sea interaction. In order to make it clear which oceanic regions are crucial to the interannual variability of the WNPSH, the research progresses in this regard in the past decade are reviewed. Based on the review, it is recognized that five oceanic regions are responsible for the interannual variability of the WNPSH in summer, including the equatorial central-eastern pacific Ocean, tropical Indian Ocean, subtropical western north pacific, the vicinity of the maritime continent, and the tropical Atlantic Ocean. The mechanisms how the sea surface temperature anomalies （SSTAs） in these regions affect the WNPSH are elaborated. The formation mechanisms for the SSTAs in these five regions are discussed. Strengths and weaknesses of the climate models in simulating and predicting the WNPSH are also documented. Finally, key scientific problems deserving further studies are proposed.

关键词： western north pacific subtropical high interannual variability air-sea interaction

Decadal Change in the Influence of the western north pacific subtropical high on Summer Rainfall over the Yangtze River Basin in the Late 1970s

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Advances in Atmospheric Sciences 2021年第11期38卷 1823-1834页

作者： Xinyu LI Riyu LU Key Laboratory of Marine Hazards Forecasting Ministry of Natural ResourcesHohai UniversityNanjing 210098China State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics Institute of Atmospheric PhysicsChinese Academy of SciencesBeijing 100029China College of Earth and Planetary Sciences University of the Chinese Academy of SciencesBeijing 100049China College of Oceanography Hohai UniversityNanjing 210098China

It is well known that on the interannual timescale,the westward extension of the western north pacific subtropical high(WNPSH)results in enhanced rainfall over the Yangtze River basin(YRB)in summer,and vice *** study identifies that this correspondence experiences a decadal change in the late *** is,the WNPSH significantly affects YRB precipitation(YRBP)after the late 1970s(P2)but not before the late 1970s(P1).It is found that enhanced interannual variability of the WNPSH favors its effect on YRB rainfall in *** the other hand,after removing the strong WNPSH cases in P2 and making the WNPSH variability equivalent to that in P1,the WNPSH can still significantly affect YRB rainfall,suggesting that the WNPSH variability is not the only factor that affects the WNPSH-YRBP *** results indicate that the change in basic state of thermal conditions in the tropical WNP provides a favorable background for the enhanced WNPSH-YRBP *** P2,the lower-tropospheric atmosphere in the tropical WNP gets warmer and wetter,and thus the meridional gradient of climatological equivalent potential temperature over the YRB is *** a result,the WNPSH-related circulation anomalies can more effectively induce YRB rainfall anomalies through affecting the meridional gradient of equivalent potential temperature over the YRB.

关键词： Yangtze River basin western north pacific subtropical high rainfall interannual relationship decadal change

Different Configurations of Interannual Variability of the western north pacific subtropical high and East Asian Westerly Jet in Summer

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Advances in Atmospheric Sciences 2021年第6期38卷 931-942页

作者： Xinyu LI Riyu LU Gen LI Key Laboratory of Marine Hazards Forecasting Ministry of Natural ResourcesHohai UniversityNanjing 210098China College of Oceanography Hohai UniversityNanjing 210098China State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics Institute of Atmospheric PhysicsChinese Academy of SciencesBeijing 100029China College of Earth and Planetary Sciences University of the Chinese Academy of SciencesBeijing 100049China

This study investigates the circulation and precipitation anomalies associated with different configurations of the western north pacific subtropical high(WNPSH)and the East Asian westerly jet(EAJ)in summer on interannual *** 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 *** out-of-phase configuration includes the residual *** find that the in-phase configuration manifests itself as a typical meridional *** instance,there is an anticyclonic(cyclonic)anomaly over the tropical western north pacific and a cyclonic(anticyclonic)anomaly over the mid-latitudes of East Asia in the lower *** circulation anomalies are more conducive to rainfall anomalies over the Yangtze River basin and south Japan than are the individual WNPSH or *** contrast,for the out-of-phase configuration,the mid-latitude cyclonic(anticyclonic)anomaly is absent,and the lower-tropospheric circulation anomalies feature an anticyclonic(cyclonic)anomaly with a large meridional ***,significant rainfall anomalies move northward to north China and the northern Korean *** results indicate that the out-of-phase configuration is associated with the developing phase of ENSO,with strong and significant sea surface temperature(SST)anomalies in the tropical central and eastern pacific which occur simultaneously during summer and persist into the following *** is sharply different from the in-phase configuration,for which the tropical SSTs are not a necessity.

关键词： western north pacific subtropical high East Asian westerly jet circulation rainfall sea surface temperature

Interdecadal Change in the Interannual Variation of the western Edge of the western north pacific subtropical high During Early Summer and the Influence of Tropical Sea Surface Temperature

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Journal of Tropical Meteorology 2022年第1期28卷 57-70页

作者： ZHAN Hong-yu CHEN Rui-dan LAN Ming Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies/School of Atmospheric Sciences Sun Yat-sen University and Southern Marine Science and Engineering Guangdong Laboratory(Zhuhai)ZhuhaiGuangdong 519082 China School of Marine Sciences Sun Yat-sen UniversityZhuhaiGuangdong 519082 China

This study reveals that the interannual variability of the western edge of the western north pacific(WNP)subtropical high(WNPSH)in early summer experienced an interdecadal decrease around ***,the zonal movement of the WNPSH and the zonal extension of the high-pressure anomaly over the WNP(WNPHA)in abnormal years possess smaller ranges after *** different influences of the tropical SSTAs are important for this interdecadal change,which exhibit slow El Nino decaying pattern before 1990 while rapid transformation from El Nino to La Nina after *** early summer tropical SSTAs and the relevant atmospheric circulation anomalies present obvious interdecadal *** 1990,the warm SSTAs over the northern Indian Ocean and southern South China Sea favor the WNPHA through eastward-propagating Kelvin wave and meridional-vertical circulation,***,the warm SSTA over the tropical central pacific induces anomalous ascent to its northwest through the Gill response,which could strengthen the anomalous descent over the WNP through meridional-vertical circulation and further favor the eastward extension of the WNPHA to central *** 1990,the warm SSTAs over the Maritime Continent and northern Indian Ocean cause the WNPHA through meridional-vertical and zonal-vertical circulation,***,the anomalous warm SSTs and ascent and the resultant anomalous descent over the WNP are located more westward and southward after 1990 than before ***,the WNPHA features narrower zonal range and less eastward extension after 1990,corresponding to the interdecadal decease in the interannual variability of the western edge of the *** the other hand,the dominant oscillation period of ENSO experienced an interdecadal reduction around 1990,contributing to the change of the El Nino SSTA associated with the anomalous WNPSH from slow decaying type to rapid transformation type.

关键词： western north pacific subtropical high interdecadal change interannual variation tropical sea surface temperature ENSO

Projected changes in the western north pacific subtropical high under six global warming targets

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Atmospheric and Oceanic Science Letters 2020年第1期13卷 26-33页

作者： FU Yuanhai GUO Dong Climate Change Research Center Institute of Atmospheric PhysicsChinese Academy of SciencesBeijingChina

The summer western north pacific subtropical high(WNPSH) has large influences on the East Asian summer climate. Many studies have focused on the projected changes in the WNPSH, but little is known about the changes under different global warming targets, such as 1.5℃ and 2.0℃. This study investigates the changes in the WNPSH under six global warming targets(1.5℃, 2.0℃, 2.5℃,3.0℃, 3.5℃, and 4.0℃) in both the mid-and lower troposphere, using the outputs of CMIP5 model in historical simulations and under Representative Concentration Pathway 8.5. The projected changes in the WNPSH, which is measured by multiple variables, show that it changes little under the 1.5℃ target in the mid-troposphere, but weakens and retreats approximately 2.5° in longitude under the 2.0℃ target. It tends to linearly weaken with warming greater than 2.5℃ and shifts eastward by approximately 6.0° in longitude by the 4.0℃ target. Meanwhile, the WNPSH intensifies and extends westward under the 1.5℃ target in the lower troposphere, but changes little with warming rising from 1.5℃ to 2.0℃. It is projected to extend westward by approximately2.0° in longitude by the 4.0℃ target.

关键词： Global warming target western north pacific subtropical high climate change

Simulation of the western north pacific subtropical high in El Ni?o decaying summers by CMIP5 AGCMs

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Atmospheric and Oceanic Science Letters 2017年第2期10卷 146-155页

作者： DONG Xiao FAN Fang-Xing LIN Ren-Ping JIN Jiang-Bo LIAN Ru-Xu International Center for Climate and Environment Sciences Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China

The performances of CMIP5 atmospheric general circulation models （AGCMs） in simulating the western north pacific subtropical high （WNPSH） in El Nino decaying summers are examined in this study. Results show that most models can reproduce the spatial pattern of both climatological and anomalous circulation associated with the WNPSH in El Nino decaying summers. Most CMIP5 AGCMs can capture the westward shift of the WNPSH in El Nino decaying summers compared with the climatological location. With respect to the sub-seasonal variation of the WNPSH, the performances of these AGCMs in reproducing the northward jump of the WNPSH are better than simulating the eastward retreat of the WNPSH from July to August. Twenty-one out of twenty-two （20 out of 22） models can reasonably reproduce the northward jump of the WNPSH in El Nino decaying summers （climatology）, while only 7 out of 22 （8 out of 22） AGCMs can reasonably reproduce the eastward retreat of the WNPSH in El Nino decaying summers （climatology）. In addition, there is a close connection between the climatological WNPSH location bias and that in El Nino decaying summers.

关键词： western north pacific subtropical high El Nino decaying summer CMIPS AGCM sub-seasonal variation

Mechanism of Regional Subseasonal Precipitation in the Strongest and Weakest East Asian Summer Monsoon Subseasonal Variation Years

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Journal of Ocean University of China 2022年第6期21卷 1411-1427页

作者： HU Haibo DENG Yuheng FANG Jiabei WANG Rongrong CMA-NJU Joint Laboratory for Climate Prediction Studies Instituted for Climate and Global Change ResearchSchool of Atmospheric ScienceNanjing UniversityNanjing 210093China Key Laboratory of Meteorological Disaster of Ministry of Education Nanjing University of Information Science and TechnologyNanjing 210044China

Using 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 Monsoon(EASM)indexes to characterize the subseasonal variability of the entire EASM *** strongest(1996)and weakest(1998)years of the subseasonal variation were revealed based on these subseasonal EASM ***,three rainfall concentration areas were defined in East Asia,and these areas were dissected by the atmospheric midlatitude jet stream axis and the position of the western north pacific subtropical high(WNPSH).Then,the subseasonal effects of the WNPSH,the South Asian high(SAH),the Mongolian Cyclone(MC),and the Boreal Summer Intraseasonal Oscillation(BSISO)on each rainfall concentration area were studied in the strongest and weakest subseasonal variation years of the *** the summer of 1998,the WNPSH and the SAH were stable in the more southern region,which not only blocked the northward progression of the BSISO but also caused the MC to advance ***,the summer of 1998 was the weakest subseasonal variability of the EASM,but with significant subseasonal precipitation episodes in the northern and central rainfall ***,in 1996,the BSISO repeatedly spread northward in the south rainfall area because of the weak intensities and northern positions of the WNPSH and the SAH,which caused significant subseasonal precipitation *** addition,MC was blocked to the north of approximately 42°N with a weak subseasonal rainfall.

关键词： East Asian Summer Monsoon Subseasonal western north pacific subtropical high Mongolian Cyclone Boreal Summer Intraseasonal Oscillation

Impacts of Two Types of northward Jumps of the East Asian Upper-tropospheric Jet Stream in Midsummer on Rainfall in Eastern China

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Advances in Atmospheric Sciences 2013年第4期30卷 1224-1234页

作者：林中达 State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics Institute of Atmospheric Physics Chinese Academy of Sciences

The East Asian upper-tropospheric jet stream （EAJS） typically jumps north of 45~N in midsummer. These annual northward jumps are mostly classified into two dominant types： the first type corresponds to the enhanced westerly to the north of the EAJS＇s axis （type A）, while the second type is related to the weakened westerly within the EAJS＇s axis （type B）. In this study, the impacts of these two types of northward jumps on rainfall in eastern China are investigated. Our results show that rainfall significantly increases in northern northeast China and decreases in the Yellow River-Huaihe River valleys, as well as in north China, during the type A jump. As a result of the type B jump, rainfall is enhanced in north China and suppressed in the Yangtze River valley. The changes in rainfall in eastern China during these two types of northward jumps are mainly caused by the northward shifts of the ascending air flow that is directly related to the EAJS. Concurrent with the type A （B） jump, the EAJS-related ascending branch moves from the Yangtze-Huai River valley to northern northeast （north） China when the EAJS＇s axis jumps from 40~N to 55~N （50~N）. Meanwhile, the type A jump also strengthens the northeast Asian low in the lower troposphere, leading to more moisture transport to northern northeast China. The type B jump, however, induces a northwestward extension of the lower-tropospheric western north pacific subtropical high and more moisture transport to north China.

关键词： northward jump East Asian upper-tropospheric jet stream eastern China rainfall northeast Asian low western north pacific subtropical high

Large-scale Circulation Control of the Occurrence of Low-level Turbulence at Hong Kong International Airport

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Advances in Atmospheric Sciences 2018年第4期35卷 435-444页

作者： Marco Y. T. LEUNG Wen ZHOU Chi-Ming SHUN Pak-Wai CHAN Guy Carpenter Asia-pacific Climate Impact Center School of Energy and Environment City University of Hong Kong Hong Kong China Hong Kong Observatory Hong Kong China

This study identifies the atmospheric circulation features that are favorable for the occurrence of low-level turbulence at Hong Kong International Airport [below 1600 feet （around 500 m）]. By using LIDAR data at the airport, turbulence and nonturbulence cases are selected. It is found that the occurrence of turbulence is significantly related to the strength of the southerly wind at 850 hPa over the South China coast. On the other hand, the east-west wihd at this height demonstrates a weak relation to the occurrence. This suggests that turbulence is generated by flow passing Lantau Island from the south. The southerly wind also transports moisture from the South China Sea to Hong Kong, reducing local stability. This is favorable for the development of strong turbulence. It is also noted that the strong southerly wind during the occurrence of low-level turbulence is contributed by an anomalous zonal gradient of geopotential in the lower troposphere over the South China Sea. This gradient is caused by the combination of variations at different timescales. These are the passage of synoptic extratropical cyclones and anticyclones and the intraseasonal variation in the western north pacific subtropical high. The seasonal variation in geopotential east of the Tibetan Plateau leads to a seasonal change in meridional wind, by which the frequency of low-level turbulence is maximized in spring and minimized in autumn.

关键词： LIDAR temperate cyclone and anticyclone western north pacific subtropical high seasonal cycle topography effect

Revisiting the Second EOF Mode of Interannual Variation in Summer Rainfall over East China

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Advances in Atmospheric Sciences 2016年第1期33卷 121-134页

作者： Zhongda LIN Qin SU Riyu LU State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics Institute of Atmospheric PhysicsChinese Academy of Sciences Department of Atmospheric Sciences Yunnan University

The second EOF（EOF2） mode of interannual variation in summer rainfall over East China is characterized by inverse rainfall changes between South China（SC） and the Yellow River-Huaihe River valleys（YH）.However,understanding of the EOF2 mode is still *** this study,the authors identify that the EOF2 mode physically depicts the latitudinal variation of the climatological summer-mean rainy belt along the Yangtze River valley（YRRB）,based on a 160-station rainfall dataset in China for the period *** latitudinal variation of the YRRB is mostly attributed to two different rainfall patterns：one reflects the seesaw（SS） rainfall changes between the YH and SC（SS pattern）,and the other features rainfall anomalies concentrated in SC only（SC pattern）.Corresponding to a southward shift of the YRRB,the SS pattern,with above-normal rainfall in SC and below-normal rainfall in the YH,is related to a cyclonic anomaly centered over the SC-East China Sea region,with a northerly anomaly blowing from the YH to SC;while the SC pattern,with above-normal rainfall in SC,is related to an anticyclonic anomaly over the western north pacific（WNP）,corresponding to an enhanced southwest monsoon over *** cyclonic anomaly,related to the SS pattern,is induced by a near-barotropic eastward propagating wave train along the Asian upper-tropospheric westerly jet,originating from the mid-high latitudes of the north *** anticyclonic anomaly,for the SC pattern,is related to suppressed rainfall in the WNP.

关键词： Yangtze River rainy belt East China summer rainfall seesaw pattern South China pattern western north pacific subtropical high extratropical wave train