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Improved ENSO simulation in regional coupled GCM using regressive correction method

Science china Earth sciences 2007年第8期50卷 1258-1265页

作者： fu weiwei1 & zhou GuangQing2 1 nansen-zhu international research center (NZC), institute of atmospheric physics, chinese academy of sciences (CAS), beijing 10002., china 2 State Key Laboratory of Numerical Modeling for atmospheric sciences and Geophysical Fluid Dynamics (LASG), institute of At-mospheric physics, CAS, beijing 10002., china 1. nansen-zhu international research center (NZC) Institute of Atmospheric Physics Chinese Academy of Sciences (CAS) Beijing 100029 China 2. State Key Laboratory of Numerical Modeling for atmospheric sciences and Geophysical Fluid Dynamics (LASG) Institute of Atmospheric Physics CAS Beijing 100029 China

A regressive correction method is presented with the primary goal of improving ENSO simulation in regional coupled GCM. It focuses on the correction of ocean-atmosphere exchanged fluxes. On the basis of numerical experiments and analysis, the method can be described as follows: first, driving the ocean model with heat and momentum flux computed from a long-term observation data set; the pro-duced SST is then applied to force the AGCM as its boundary condition; after that the AGCM’s simula-tion and the corresponding observation can be correlated by a linear regressive formula. Thus the re-gressive correction coefficients for the simulation with spatial and temporal variation could be obtained by linear fitting. Finally the coefficients are applied to redressing the variables used for the calculation of the exchanged air-sea flux in the coupled model when it starts integration. This method together with the anomaly coupling method is tested in a regional coupled model, which is composed of a global grid-point atmospheric general circulation model and a high-resolution tropical Pacific Ocean model. The comparison of the results shows that it is superior to the anomaly coupling both in reducing the coupled model ‘climate drift’ and in improving the ENSO simulation in the tropical Pacific Ocean.

关键词： anomaly coupling regressive correction method regional coupled model ENSO simulation

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Sea surface temperature east of Australia:A predictor of tropical cyclone frequency over the western North Pacific?

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chinese Science Bulletin 2011年第2期56卷 196-201页

作者： zhou BoTao 1,2 & CUI Xuan 3 1 National Climate center,china Meteorological Administration,beijing 100081,china 2 nansen-zhu international research center,institute of atmospheric physics,chinese academy of sciences,beijing 10002.,china 3 National Meteorological center,china Meteorological Administration,beijing 100081,china National Climate center China Meteorological Administration Beijing China nansen-zhu international research center Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China National Meteorological center China Meteorological Administration Beijing China

The relationship between sea surface temperature (SST) east of Australia and tropical cyclone frequency over the western North Pacific (WNPTCF) is analyzed by use of observation *** WNPTCF from June to October is correlated negatively to spring SST east of *** the spring SST is in the positive phase,a cyclonic circulation anomaly in the upper troposphere and an anticyclonic circulation anomaly in the lower troposphere prevail over the western North Pacific from June to October,concurrent with an anomalous atmospheric subsidence and an enlarged vertical zonal wind *** conditions are unfavorable for tropical cyclone genesis,and thus WNPTCF *** negative phase of the spring SST east of Australia leads to more tropical cyclones over the western North *** spring SST east of Australia may give rise to simultaneous change in tropical atmospheric circulation via the teleconnection wave train,and then subsequently affect atmospheric circulation variation over the western North Pacific.

关键词：热带气旋北太平洋澳大利亚西部海面温度热带大气环流预测频率

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Modeling the impact of Australian Plate drift on Southern Hemisphere climate and environment

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chinese Science Bulletin 2005年第14期50卷 1495-1502页

作者： zhou Botao1,5, ZHAO Ping2, JIAN Zhimin3 & HE Jinhai4 1. nansen-zhu international research center, institute of atmospheric physics, chinese academy of sciences, beijing 10002., china 2. institute of Climate and Environment, chinese academy of Meteoro- logical sciences, beijing 100081, china 3. Laboratory of Marine Geology, Tongji University, Shanghai 200092, china 4. Department of atmospheric sciences, Nanjing institute of Meteorol- ogy, Nanjing 210044, china 5. Graduate School of the chinese academy of sciences, beijing 100039, china nansen-zhu international research center Institute of Atmospheric Physics Chinese Academy of Sciences Beijing 100029 China Graduate School of the chinese academy of sciences Beijing 100039 China institute of Climate and Environment Chinese Academy of Meteorological Sciences Beijing 100081 China Laboratory of Marine Geology Tongji University Shanghai 200092 China Department of atmospheric sciences Nanjing Institute of Meteorology Nanjing 210044 China

Using a global atmosphere-ocean coupled model with the present-day and 14 MaB.P. oceanic topogra- phy respectively, two experiments are implemented to inves- tigate the effect of different locations of Australian Plate on the atmospheric circulation in middle-high latitudes of the Southern Hemisphere. The results show that when Austra- lian Plate lay south at 14 MaB.P., both anticyclone circula- tions in the subtropical oceans and cyclone circulation around 60°-70°S are strengthened. Subtropical highs and circumpolar low pressure appear stronger, which results in much stronger Antarctic Oscillation and shorter period of Antarctic Oscillation Index (AOI) at 14 MaB.P. The rainfall and the surface air temperature also change correspondingly. The precipitation decreases around 40°S and increases around 60°-70°S, and the surface air temperature rises in high latitudes of the South Pacific and descends over the Weddell Sea and its north side. Besides, due to the changes of the temperatures and winds, Antarctic sea ice coverage also changes with its increasing in the Ross Sea and its west re- gions and decreasing in the Weddell Sea.

关键词：半球气候地球环球澳大利亚漂流物海洋地形学

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A three-dimensional variational ocean data assimilation system:Scheme and preliminary results

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Science china Earth sciences 2006年第11期49卷 1212-1222页

作者： zhu Jiang1,2, zhou Guangqing1, YAN Changxiang1, fu weiwei1 & YOU Xiaobao1,3 1. international center for Climate and Environment sciences, institute of atmospheric physics, chinese academy of sciences, beijing 10002., china 2. Jiangsu Key Laboratory of Meteorological Disaster, Nanjing University of Information Science and Technology, Nanjing 210044, china 3. beijing institute of Applied Meteorology, beijing 10002., china 1. international center for Climate and Environment sciences Institute of Atmospheric Physics Chinese Academy of Sciences Beijing 100029 China 2. Jiangsu Key Laboratory of Meteorological Disaster Nanjing University of Information Science and Technology Nanjing 210044 China 3. beijing institute of Applied Meteorology Beijing 100029 China

A new 3DVAR-based Ocean Variational Analysis System (OVALS) is developed. OVALS is capable of assimilating in situ sea water temperature and salinity observations and satellite altimetry data. As a component of OVALS, a new variational scheme is proposed to assimilate the sea surface height data. This scheme considers both the vertical correlation of background errors and the nonlinear temperature-salinity relationship which is derived from the generalization of the linear balance constraints to the nonlinear in the 3DVAR. By this scheme, the model temperature and salinity fields are directly adjusted from the altimetry data. Additionally, OVALS can assimilate the temperature and salinity profiles from the ARGO floats which have been implemented in recent years and some temperature and salinity data such as from expendable bathythermograph, moored ocean buoys, etc. A 21-year assimilation experiment is carried out by using OVALS and the Tropical Pacific circulation model. The results show that the assimilation system may effectively improve the estimations of temperature and salinity by assimilating all kinds of observations. Moreover, the root mean square errors of temperature and salinity in the upper depth less than 420 m reach 0.63℃ and 0.34 psu.

关键词： data assimilation, 3DVAR, sea surface height, ARGO floats.

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Distinct Interannual Variability and Physical Mechanisms of Snowfall Frequency over the Eurasian Continent during Autumn and Winter

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Advances in atmospheric sciences 2024年第10期41卷 1969-1983,I0011-I0013页

作者： Siyu zhou Bo SUN Huijun WANG Yi ZHENG Jiarui CAI Huixin LI Botao zhou Collaborative Innovation center on Forecast and Evaluation of Meteorological Disasters/Key Laboratory of Meteorological Disasters Ministry of Education/Joint International Research Laboratory of Climate and Environment ChangeNanjing University of Information Science and TechnologyNanjing 210044China Southern Marine Science and Engineering Guangdong Laboratory Zhuhai 519080China nansen zhu international research Centre Institute of Atmospheric PhysicsChinese Academy of SciencesBeijing 100029China

This study investigates the dominant modes of interannual variability of snowfall frequency over the Eurasian continent during autumn and winter,and explores the underlying physical *** first EOF mode(EOF1)of snowfall frequency during autumn is mainly characterized by positive anomalies over the Central Siberian Plateau(CSP)and Europe,with opposite anomalies over Central Asia(CA).EOF1 during winter is characterized by positive anomalies in Siberia and negative anomalies in Europe and East Asia(EA).During autumn,EOF1 is associated with the anomalous sea ice in the Kara–Laptev seas(KLS)and sea surface temperature(SST)over the North *** sea ice in the KLS may cause an increase in the meridional air temperature gradient,resulting in increased synoptic-scale wave activity,thereby inducing increased snowfall frequency over Europe and the *** increases of both sea ice in the KLS and SST in the North Atlantic may stimulate downstream propagation of Rossby waves and induce an anomalous high in CA corresponding to decreased snowfall *** contrast,EOF1 is mainly affected by the anomalous atmospheric circulation during *** the positive phase of the North Atlantic Oscillation(NAO),an anomalous deep cold low(warm high)occurs over Siberia(Europe)leading to increased(decreased)snowfall frequency over Siberia(Europe).The synoptic-scale wave activity excited by the positive NAO can induce downstream Rossby wave propagation and contribute to an anomalous high and descending motion over EA,which may inhibit *** NAO in winter may be modulated by the Indian Ocean dipole and sea ice in the Barents-Kara-Laptev Seas in autumn.

关键词： snowfall frequency Eurasian continent sea ice atmospheric circulation interannual variability Indian Ocean dipole

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Causes of the Intraseasonal SST Variability in the Tropical Indian Ocean

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atmospheric and Oceanic Science Letters 2008年第1期1卷 18-23页

作者： Tim Li Francis Tam Xiouhua fu zhou Tian-Jun zhu Wei-Jun IPRC and Department of Meteorology University of Hawaii at Manoa Honolulu Hawaii USA institute of atmospheric physics Chinese Academy of Sciences Beijing 100029 China Joint Climate institute of CMA ＆ NUIST Nanjing University of Information Science ＆ Technology Nanjing 210044 China

Satellite observations reveal a much stronger intraseasonal sea surface temperature （SST） variability in the southern Indian Ocean along 5-10°S in boreal winter than in boreal summer. The cause of this seasonal dependence is studied using a 2 1/2-layer ocean model forced by ERA-40 reanalysis products during 1987-2001. The simulated winter-summer asymmetry of the SST variability is consistent with the observed. A mixed-layer heat budget is analyzed. Mean surface westerlies along the ITCZ （5-10°S） in December-January-February （DJF） leads to an increased （decreased） evaporation in the westerly （easterly） phase of the intraseasonal oscillation （ISO）, during which convection is also enhanced （suppressed）. Thus the anomalous shortwave radiation, latent heat flux and entrainment effects are all in phase and produce strong SST signals. During June-July-August （JJA）, mean easterlies prevail south of the equator. Anomalies of the shortwave radiation tend to be out of phase to those of the latent heat flux and ocean entrainment. This mutual cancellation leads to a weak SST response in boreal summer. The resultant SST tendency is further diminished by a deeper mixed layer in JJA compared to that in DJF. The strong intraseasonal SST response in boreal winter may exert a delayed feedback to the subsequent opposite phase of ISO, implying a two-way air-sea interaction scenario on the intraseasonal timescale.

关键词： SST ISO shortwave radiation latent heatflux ocean entrainment

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Intercomparison of the South Asian High in NCEP1, NCEP2, and ERA-40 Reanalyses and in Station Observations

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atmospheric and Oceanic Science Letters 2012年第3期5卷 189-194页

作者： fu Jian-Jian LI Shuanglin nansen-zhu international research Centre(NZC) Institute of Atmospheric PhysicsChinese Academy of SciencesBeijing 100029China

The South Asian Highs (SAHs) at 100 hPa over china in the three reanalysis datasets NCEP1, NCEP2, and ERA-40 are evaluated by using station observation data. The results demonstrate a substantial discrepancy even between the reanalyses. First, the data of the three reanalyses generally underestimate the intensity of the SAH in the china domain. Second, there are interdecadal changes in the SAH, with highs in the 1960s and 1980s and lows in the 1970s, 1990s, and 2000s. This interdecadal variation of the SAH can be well depicted with NCEP1 data, but the high in the 1980s is missed by ERA-40. The NCEP2 corresponds well with NCEP 1 and captures the decreasing trend after 1979. furthermore, the NCEP1 reanalysis overestimates the interdecadal changes of SAH, while ERA-40 underestimates the interdecadal changes. This work suggests that much caution should be exerted when the reanalysis datasets are adopted to study the interdecadal variability of SAH.

关键词： South Asian High interdecadal change reanalysis datasets station observation

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Model Evaluation and Projection on the Linkage between Hadley Circulation and atmospheric Background Related to the Tropical Cyclone Frequency over the Western North Pacific

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atmospheric and Oceanic Science Letters 2012年第6期5卷 473-477页

作者： zhou Bo-Tao National Climate center Beijing 100081 China nansen-zhu international research center Institute of Atmospheric Physics Chinese Academy of Sciences Beijing 100029 China

The performance of climate models in simulating the linkage of the spring Hadley circulation (HC) to the vertical zonal wind shear and atmospheric divergence in the lower and upper troposphere, which are related to the tropical cyclone frequency over the western North Pacific (WNPTCF) during June-September (JJAS), is evaluated on the basis of the 20th century climate simulations (20C3M). It is found that four models can simulta-neously reproduce the pattern revealed in the observation, with the spring HC in the Northern Hemisphere being positively correlated to the vertical zonal wind shear in the major tropical cyclone (TC) genesis region and negatively (positively) correlated to the atmospheric diver- gence in the upper (lower) troposphere over the western North Pacific (WNP) in the following JJAS. These four models are further used to project their relationship in the late 21st century under the A1B scenario. The results show that the association of spring HC with the vertical zonal wind shear and the upper-and lower-tropospheric divergence over the WNP will weaken in the late 21st century, thereby resulting in a weak relationship between the spring HC and the JJAS WNPTCF.

关键词： Hadley circulation atmospheric circulation tropical cyclone assessment projection

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把握机会窗口期减缓气候变化对中国居民健康影响

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科学通报 2023年第15期68卷 1899-1905页

作者：蔡闻佳张弛张诗卉艾思奇白玉琪鲍俊哲常楠陈彬陈慧琪程亮亮崔学勤戴瀚程 Bawuerjiang Danna 底骞董伟董文轩窦德景范维澄范星房小怡高仝高源耿阳关大博郭亚菲 Ian Hamilton 胡艺馨华峻翊黄存瑞黄弘黄建斌蒋俏蕾姜晓朋柯丕煜 Gregor Kiesewetter Pete Lampard 李传玺李瑞奇李双利梁璐林波荣林华亮刘欢刘起勇刘小波刘心远刘昱甫刘钊刘竹楼书含鲁晨曦罗勇罗震宇马伟 Alice McGushin 牛彦麟任超阮增良 Wolfgang Schöpp 单钰理苏婧孙韬淳王灿王琼文三妹谢杨熊辉徐冰徐朦颜钰杨军杨廉平杨秀俞乐岳玉娟曾仪娉张镜张少辉张曜张仲宸赵继尧赵亮赵梦真赵琦赵哲周景博朱征宏陈冯富珍宫鹏清华大学地球系统科学系北京100084 北京理工大学管理与经济学院北京100081 中山大学公共卫生学院广州510080 郑州大学公共卫生学院郑州450001 南京医科大学公共卫生学院南京211166 北京师范大学环境学院北京100875 北京大学环境工程学院北京100871 清华大学新闻与传播学院北京100084 清华大学万科公共卫生学院北京100084 浙江大学地球科学学院杭州310058 清华大学公共安全研究所北京100084 清华大学工程物理系北京100084 百度研究院北京100091 山东师范大学环境与生态研究院济南250013 中国气象科学研究院气象影响与风险研究中心北京100086 山东师范大学商学院济南250013 中国疾病预防控制中心传染病预防控制所传染病预防控制国家重点实验室北京102206 清华大学建筑学院北京100084 中国疾病预防控制中心环境与人群健康重点实验室环境与健康相关产品安全所北京102206 Energy institute University College LondonLondon WC1E 6BTUK 南方科技大学统计与数据科学系深圳518055 香港大学建筑学院中国香港999077 世界卫生组织驻华代表处北京100600 Pollution Management research Group EnergyClimateand Environment ProgramInternational Institute for Applied Systems Analysis(IIASA)Schlossplatz 1-A-2361 LaxenburgAustria Department of Health sciences University of YorkYork YO105DDCanada 山东大学齐鲁医学院公共卫生学院流行病学系济南250002 中国科学技术大学计算机科学与技术学院合肥230027 Department of Geography and the Environment University of North TexasDenton TX 76203-5017USA 清华大学环境学院北京100084 Geography College of Life and Environmental SciencesUniversity of ExeterExeter EX12LUUK 山东大学气候变化与健康研究中心济南250002 institute for Global Health University College LondonLondon WC1H 0ALUK School of Geography Earth and Environmental SciencesUniversity of BirminghamBirmingham B152TTUK 清华大学人文学院北京100084 北京航空航天大学经济与管理学院北京100083 香港科技大学(广州)信息枢纽人工智能学域广州511443 暨南大学环境与气候研究所广州510632 清华大学气候变化与可持续发展研究院北京100084 清华大学苏世民学院北京100084 清华大学体育学部北京100084 中国科学院大气物理研究所大气科学和地球流体力学数值模拟国家重点实验室北京100029 香港大学地球科学系和地理系中国香港999077

随着中国总人口的不断增加以及改革开放以来经济的飞速发展,中国面临来自气候变化的健康威胁也在不断上升.与此同时,中国也处于一个独特的机遇窗口期,如果能够有效应对气候变化带来的健康风险,将造福今后几代人的健康.反之,如果没有及... 详细信息

随着中国总人口的不断增加以及改革开放以来经济的飞速发展,中国面临来自气候变化的健康威胁也在不断上升.与此同时,中国也处于一个独特的机遇窗口期,如果能够有效应对气候变化带来的健康风险,将造福今后几代人的健康.反之,如果没有及时、充分的应对措施,气候变化对中国居民健康和生命的威胁将与日俱增.为了推动更及时且有利于改善人群健康的气候应对行动,由清华大学牵头建立的柳叶刀倒计时亚洲中心在全球柳叶刀倒计时工作的基础上[1,2],从2020年开始,聚焦气候变化对中国人群健康的影响进行全面且系统的评估[3,4].

关键词：减缓气候变化人群健康柳叶刀居民健康窗口期倒计时应对措施把握机会

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