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| 1 | Towards reliable Arctic sea ice prediction using multivariate data assimilation显示文摘Rapid declines in Arctic sea ice have captured attention and pose significant challenges to a variety of stakeholders. There is a rising demand for Arctic sea ice prediction at daily to seasonal time scales, which is partly a sea ice initial condition problem. Thus, a multivariate data assimilation that integrates sea ice observations to generate realistic and skillful model initialization is needed to improve predictive skill of Arctic sea ice. Sea ice data assimilation is a relatively new research area. In this review paper, we focus on two challenges for implementing multivariate data assimilation systems for sea ice forecast. First, to address the challenge of limited spatiotemporal coverage and large uncertainties of observations, we discuss sea ice parameters derived from satellite remote sensing that(1) have been utilized for improved model initialization, including concentration, thickness and drift, and(2) are currently under development with the potential for enhancing the predictability of Arctic sea ice, including melt ponds and sea ice leads. Second, to strive to generate the ‘‘best' estimate of sea ice initial conditions by combining model simulations/forecasts and observations, we review capabilities and limitations of different data assimilation techniques that have been developed and used to assimilate observed sea ice parameters in dynamical models. | Jiping Liu Zhiqiang Chen Yongyun Hu Yuanyuan Zhang Yifan Ding Xiao Cheng Qinghua Yang Lars Nerger Gunnar Spreen Radley Horton Jun Inoue Chaoyuan Yang Ming Li Mirong Song | 2019 | Science Bulletin2019，64，1： | 10 |
| 2 | Widening and weakening of the Hadley circulation under global warming显示文摘The Hadley circulation is one of the most important atmospheric circulations.Widening of the Hadley circulation has drawn extensive studies in the past decade.The key concern is that widening of the Hadley circulation would cause poleward shift of the subtropical dry zone.Various metrics have been applied to measure the widening of the tropics.What are responsible for the observed widening trends of the Hadley circulation? How anthropogenic and natural forcings caused the widening? How the widening results in regional climatic effects? These are the major questions in studing the widening of the Hadley circulation.While both observations and simulations all show widening of the Hadley circulation in the past few decades,there are no general agreements of changes in the strength of the Hadley circulation.Although some reanalysis datasets show strengthening of the Hadley circulation,it was shown that the strengthening trend could be artificial,and simulations show weakening of the Hadley circulation for global greenhouse warming.In the present paper,we shall briefly review the major progresses of studies in trends in width and strength of the Hadley circulation.We address answers to these questions,clarify inconsistent results,and propose ideas for future studies. | Yongyun Hu Han Huang Chen Zhou | 2018 | Science Bulletin2018，63，10： | 7 |
| 3 | Review of Chinese atmospheric science research over the past 70 years: Synoptic meteorology显示文摘Synoptic meteorology is a branch of meteorology that uses synoptic weather observations and charts for the diagnosis,study,and forecasting of weather.Weather refers to the specific state of the atmosphere near the Earth’s surface during a short period of time.The spatial distribution of meteorological elements in the atmosphere can be represented by a variety of transient weather phenomena,which are caused by weather systems of different spatial and temporal scales.Weather is closely related to people’s life,and its development and evolution have always been the focus of atmospheric scientific research and operation.The development of synoptic meteorology is closely related to the development of observation systems,dynamical theories and numerical models.In China,observation networks have been built since the early 1950 s.Up to now,a comprehensive meteorological observation systembased on ground,air and space has been established.In particular,the development of a new generation of dense radar networks,the development of the Fengyun satellite series and the implementation of a series of large field experiments have brought our understanding of weather from large-scale environment to thermal dynamics,cloud microphysical structure and evolution characteristics of meso and micro-scale weather systems.The development of observation has also promoted the development of theory,numerical model and simulation.In the early days,China mainly used foreign numerical models.Lately,China has developed numerical model systems with independent intellectual property rights.Based on the results of high-resolution numerical simulations,in-depth understanding of the initiation and evolution mechanism and predictability of weather at different scales has been obtained.Synoptic meteorology has gradually changed from an initially independent development to a multidisciplinary approach,and the interaction between weather and the change of climate and environment has become a hot and frontier topic in atmospheric science.This paper reviews the important scientific and technological achievements made in China over the past 70 years in the fields of synoptic meteorology based on the literatures in China and abroad,from six aspects respectively including atmospheric dynamics,synoptic-scale weather,typhoon and tropical weather,severe convective weather,numerical weather prediction and data assimilation,weather and climate,atmospheric physics and atmospheric environment. | Zhiyong MENG Fuqing ZHANG Dehai LUO Zhemin TAN Juan FANG Jianhua SUN Xueshun SHEN Yunji ZHANG Shuguang WANG Wei HAN Kun ZHAO Lei ZHU Yongyun HU Huiwen XUE Yaping MA Lijuan ZHANG Ji NIE Ruilin ZHOU Sa LI Hongjun LIU Yuning ZHU | 2019 | Science China Earth Sciences2019，62，12： | 7 |
| 4 | Surface and tropospheric ozone trends in the Southern Hemisphere since 1990: possible linkages to poleward expansion of the Hadley circulation显示文摘Increases in free tropospheric ozone over the past two decades are mainly in the Northern Hemisphere that have been widely documented,while ozone trends in the Southern Hemisphere(SH)remain largely unexplained.Here we first show that in-situ and satellite observations document increases of tropospheric ozone in the SH over 1990–2015.We then use a global chemical transport model to diagnose drivers of these trends.We find that increases of anthropogenic emissions(including methane)are not the most significant contributors.Instead,we explain the trend as due to changes in meteorology,and particularly in transport patterns.We propose a possible linkage of the ozone increases to meridional transport pattern shifts driven by poleward expansion of the SH Hadley circulation(SHHC).The SHHC poleward expansion allows more downward transport of ozone from the stratosphere to the troposphere at higher latitudes,and also enhances tropospheric ozone production through stronger lifting of tropical ozone precursors to the upper troposphere.These together may lead to increasing tropospheric ozone in the extratropical SH,particularly in the middle/upper troposphere and in austral autumn.Poleward expansion of the Hadley circulation is partly driven by greenhouse warming,and the associated increase in tropospheric ozone potentially provides a positive climate feedback amplifying the warming that merits further quantification. | Xiao Lu Lin Zhang Yuanhong Zhao Daniel J.Jacob Yongyun Hu Lu Hu Meng Gao Xiong Liu Irina Petropavlovskikh Audra McClure-Begley Richard Querel | 2019 | Science Bulletin2019，64，6： | 7 |
| 5 | Coagulation factors VII, IX and X are effective antibacterial proteins against drug-resistant Gram-negative bacteria显示文摘Infections caused by drug-resistant“superbugs”pose an urgent public health threat due to the lack of effective drugs;however, certain mammalian proteins with intrinsic antibacterial activity might be underappreciated. Here, we reveal an antibacterial property against Gram-negative bacteria for factors VII, IX and X, three proteins with well-established roles in initiation of the coagulation cascade. These factors exert antibacterial function via their light chains (LCs). Unlike many antibacterial agents that target cell metabolism or the cytoplasmic membrane, the LCs act by hydrolyzing the major components of bacterial outer membrane, lipopolysaccharides, which are crucial for the survival of Gram-negative bacteria. The LC of factor VII exhibits in vitro efficacy towards all Gram-negative bacteria tested, including extensively drug-resistant (XDR) pathogens, at nanomolar concentrations. It is also highly effective in combating XDR Pseudomonas aeruginosa and Acinetobacter baumannii infections in vivo. Through decoding a unique mechanism whereby factors VII, IX and X behave as antimicrobial proteins, this study advances our understanding of the coagulation system in host defense, and suggests that these factors may participate in the pathogenesis of coagulation disorder-related diseases such as sepsis via their dual functions in blood coagulation and resistance to infection. Furthermore, this study may offer new strategies for combating Gram-negative “superbugs”. | Jinwu Chen Xiaojie Li Ling Li Ting Zhang Qing Zhang Fangming Wu Diyue Wang Hongze Hu Changlin Tian Dongsheng Liao Liang Zhao Danxia Song Yongyun Zhao Chuanfang Wu Xu Song | 2019 | Cell Research2019，29，9： | 6 |
| 6 | Extremely cold and persistent stratospheric Arctic vortex in the winter of 2010-2011显示文摘Record ozone loss was observed in the stratospheric Arctic in the spring of 2011. In the present work, we show observational evidence that the record loss of Arctic ozone is due to the extremely cold and persistent stratospheric polar vortex in the winter of 2010-2011. The polar vortex was as usual in early winter, but was intensified twice in middle January and middle February, respectively, and remained anomalously strong and stable until early April, 2011. Record low polar temperatures and record high subpolar zonal winds occurred in February and March. Stratospheric wave activity was anomalously weak because waves were refracted equatorward by the anomalously strong polar night jet. With such an extremely cold and isolated environment, Arctic stratospheric ozone was largely depleted in March and early April, 2011. Corresponding to Arctic ozone depletion, the stratospheric Northern-Hemisphere Annular Mode (NAM) displayed anomalously strong high-polarity, and the positive stratospheric NAM propagated downward and led to anomalously strong positive NAM in the troposphere and near the surface. | HU YongYun XIA Yan | 2013 | Chinese Science Bulletin2013，58，25： | 5 |
| 7 | Stratospheric Ozone-induced Cloud Radiative Effects on Antarctic Sea Ice显示文摘Recent studies demonstrate that the Antarctic Ozone Hole has important influences on Antarctic sea ice.While most of these works have focused on effects associated with atmospheric and oceanic dynamic processes caused by stratospheric ozone changes,here we show that stratospheric ozone-induced cloud radiative effects also play important roles in causing changes in Antarctic sea ice.Our simulations demonstrate that the recovery of the Antarctic Ozone Hole causes decreases in clouds over Southern Hemisphere(SH)high latitudes and increases in clouds over the SH extratropics.The decrease in clouds leads to a reduction in downward infrared radiation,especially in austral autumn.This results in cooling of the Southern Ocean surface and increasing Antarctic sea ice.Surface cooling also involves ice-albedo feedback.Increasing sea ice reflects solar radiation and causes further cooling and more increases in Antarctic sea ice. | Yan XIA Yongyun HU Jiping LIU Yi HUANG Fei XIE Jintai LIN | 2020 | Advances in Atmospheric Sciences2020，37，5： | 3 |
| 8 | Advances in Researches on the Middle and Upper Atmosphere in 2008-2010显示文摘This paper summarizes the results of the researches on the middle and upper atmosphere obtained by Chinese scientists in 2008-2010.The focuses are specifically placed on the researches being associated with ground-based observation capability development,dynamical processes,the property of atmospheric circulation and the chemistry-climate coupling of the middle atmospheric layers. | Chen Zeyu Chen Hongbin Lue Daren Xu Jiyao Chen Wen Tian Wenshou Ren Rongcai Hu Yongyun Huang Kaiming | 2010 | 空间科学学报2010，30，5： | 2 |
| 9 | Lower Stratospheric Water Vapor Variations Diagnosed from Satellite Observations,Reanalysis Data,and a Chemistry-Climate Model显示文摘Stratospheric water vapor variations,which may play an important role in surface climate,have drawn extensive studies.Here,the variation in stratospheric water vapor is investigated by using data from observations of the Microwave Limb Sounder(MLS)on the Aura satellite,from the ECMWF Interim Reanalysis(ERAI),and simulations by the Whole Atmosphere Community Climate Model(WACCM).We find that the differences of annual mean stratospheric water vapor among these datasets may be partly caused by the differences in vertical transports.Using budget analysis,we find that the upward transport of water vapor at 100 h Pa is mainly located over the Pacific warm pool region and South America in the equatorial tropics in boreal winter and over the southeast of the South Asian high and south of North America in boreal summer.It is found that temperature averaged over regions with upward transport is a better indicator of interannual variability of tropical mean stratospheric water vapor than the tropical mean temperature.It seems that the distributions of the seasonal cycle amplitude of lower stratospheric water vapor in the tropics can also be impacted by the vertical transport.The radiative effects of the interannual changes in water vapor in the lowermost stratosphere are underestimated by approximately 29%in both ERAI and WACCM compared to MLS,although the interannual variations of water vapor in the lowermost stratosphere are dramatically overestimated in ERAI and WACCM.The results here indicate that the radiative effect of long-term changes in water vapor in the lowermost stratosphere may be underestimated in both ERAI and WACCM simulations. | Yan XIA Yi HUANG Yongyun HU Jun YANG | 2021 | Journal of Meteorological Research2021，35，4： | 1 |
| 10 | Enhancing the capabilities of biosafety laboratories through the established accreditation system:Development of the biosafety laboratory accreditation system in China显示文摘Accreditation is now widely used to attest for laboratory competence.Although accreditation was originally used to assess products in testing laboratories and still plays an increasingly important role in international trade,it has been expanded to include laboratories in many social fields,including forensic science,medicine,and animal quarantine reference.The accreditation process provides basic requirements for achieving global recognition for laboratory reports.This paper introduces the concept of accreditation and discusses the origins and development of the accreditation system in Chinese biosafety laboratories.This study also reveals the important role of this system in national biosafety management through an examination of the 14-year development of the Chinese biosafety laboratory accreditation system. | Peijun Zhai Rong Wang Yongyun Zhou Dongmei Hu Junyan li Yali Zhou | 2019 | Journal of Biosafety and Biosecurity2019，1，2： | 1 |
| 11 | Record Arctic Ozone Loss in Spring 2020 is Likely Caused by North Pacific Warm Sea Surface Temperature Anomalies显示文摘Record ozone loss was observed in the Arctic stratosphere in spring 2020.This study aims to determine what caused the extreme Arctic ozone loss.Observations and simulation results are examined in order to show that the extreme Arctic ozone loss was likely caused by record-high sea surface temperatures(SSTs)in the North Pacific.It is found that the record Arctic ozone loss was associated with the extremely cold and persistent stratospheric polar vortex over February-April,and the extremely cold vortex was a result of anomalously weak planetary wave activity.Further analysis reveals that the weak wave activity can be traced to anomalously warm SSTs in the North Pacific.Both observations and simulations show that warm SST anomalies in the North Pacific could have caused the weakening of wavenumber-1 wave activity,colder Arctic vortex,and lower Arctic ozone.These results suggest that for the present-day level of ozone-depleting substances,severe Arctic ozone loss could form again,as long as certain dynamic conditions are satisfied. | Yan XIA Yongyun HU Jiankai ZHANG Fei XIE Wenshou TIAN | 2021 | Advances in Atmospheric Sciences2021，38，10： | 1 |
| 12 | Advances in the Researches of the Middle and Upper Atmosphere in China in 2012–2014显示文摘In this report we summarize the research results by Chinese scientists in 2012–2014. The focuses are placed on the researches of the middle and upper atmosphere, specifically the researches related to ground-based observation capability development, dynamical processes, the property of circulation and chemistry-climate coupling of the middle atmospheric layers. | CHEN Zeyu CHEN Hongbin XU Jiyao BIAN Jianchun QIE Xiushu Lü Daren CHEN Wen REN Rongcai ZHANG Shaodong DOU Xiankang LI Tao HU Xiong HU Yongyun TIAN Wenshou | 2014 | 空间科学学报2014，34，5： | 0 |
| 13 | Attribution of Biases of Interhemispheric Temperature Contrast in CMIP6 Models显示文摘One of the basic characteristics of Earth's modern climate is that the Northern Hemisphere(NH) is climatologically warmer than the Southern Hemisphere(SH). Here, model performances of this basic state are examined using simulation results from 26 CMIP6 models. Results show that the CMIP6 models underestimate the contrast in interhemispheric surface temperatures on average(0.8 K for CMIP6 mean versus 1.4 K for reanalysis data mean), and that there is a large intermodel spread, ranging from -0.7 K to 2.3 K. A box model energy budget analysis shows that the contrast in interhemispheric shortwave absorption at the top of the atmosphere, the contrast in interhemispheric greenhouse trapping, and the crossequatorial northward ocean heat transport, are all underestimated in the multimodel mean. By examining the intermodel spread, we find intermodel biases can be tracked back to biases in midlatitude shortwave cloud forcing in AGCMs. Models with a weaker interhemispheric temperature contrast underestimate the shortwave cloud reflection in the SH but overestimate the shortwave cloud reflection in the NH, which are respectively due to underestimation of the cloud fraction over the SH extratropical ocean and overestimation of the cloud liquid water content over the NH extratropical continents.Models that underestimate the interhemispheric temperature contrast exhibit larger double ITCZ biases, characterized by excessive precipitation in the SH tropics. Although this intermodel spread does not account for the multimodel ensemble mean biases, it highlights that improving cloud simulation in AGCMs is essential for simulating the climate realistically in coupled models. | Shiyan ZHANG Yongyun HU Jiankai ZHANG Yan XIA | 2024 | Advances in Atmospheric Sciences2024，41，2： | 0 |
| 14 | The Walker Circulation shaped by tectonics显示文摘The Walker Circulation is a thermally driven tropical atmospheric circulation in the longitudinal direction.At present,the ascending branch of the Walker Circulation is over the warm pool in the tropical western Pacific and the descending branch is over the tropical eastern Pacific where sea-surface temperatures(SSTs)are cooler.How could the Walker Circulation be a few tens of million years ago(Ma)?How did it evolve over tectonic time scales? | Yongyun Hu | 2021 | National Science Review2021，8，5： | 0 |
| 15 | Assessment of Snow Depth over Arctic Sea Ice in CMIP6 Models Using Satellite Data显示文摘Snow depth over sea ice is an essential variable for understanding the Arctic energy budget.In this study,we evaluate snow depth over Arctic sea ice during 1993-2014 simulated by 31 models from phase 6 of the Coupled Model Intercomparison Project(CMIP6)against recent satellite retrievals.The CMIP6 models capture some aspects of the observed snow depth climatology and variability.The observed variability lies in the middle of the models’simulations.All the models show negative trends of snow depth during 1993-2014.However,substantial spatiotemporal discrepancies are identified.Compared to the observation,most models have late seasonal maximum snow depth(by two months),remarkably thinner snow for the seasonal minimum,an incorrect transition from the growth to decay period,and a greatly underestimated interannual variability and thinning trend of snow depth over areas with frequent occurrence of multi-year sea ice.Most models are unable to reproduce the observed snow depth gradient from the Canadian Arctic to the outer areas and the largest thinning rate in the central Arctic.Future projections suggest that snow depth in the Arctic will continue to decrease from 2015 to 2099.Under the SSP5-8.5 scenario,the Arctic will be almost snow-free during the summer and fall and the accumulation of snow starts from January.Further investigation into the possible causes of the issues for the simulated snow depth by some models based on the same family of models suggests that resolution,the inclusion of a hightop atmospheric model,and biogeochemistry processes are important factors for snow depth simulation. | Shengzhe CHEN Jiping LIU Yifan DING Yuanyuan ZHANG Xiao CHENG Yongyun HU | 2021 | Advances in Atmospheric Sciences2021，38，2： | 0 |
| 16 | Advances in the Researches of the Middle and Upper Atmosphere in China显示文摘In this report we summarize the research results by Chinese scientists in 2018–2020.The focuses are placed on the researches of the middle and upper atmosphere,specifically the researches on atmospheric structure and composition,climate and chemistry-climate coupling and climate modelling,dynamics in particular those inducing the coupling of the atmospheric layers. | CHEN Zeyu CHEN Hongbin XU Jiyao HUANG Kaiming XUE Xianghui HU Dingzhu CHEN Wen YANG Guotao TIAN Wenshou HU Yongyun XIA Yan | 2020 | 空间科学学报2020，40，5： | 0 |
| 17 | Erratum to:Stratospheric Ozone-induced Cloud Radiative Effects on Antarctic Sea Ice显示文摘The article“Stratospheric Ozone-induced Cloud Radiative Effects on Antarctic Sea Ice”,written by Yan XIA,Yongyun HU,Jiping LIU,Yi HUANG,Fei XIE,and Jintai LIN was originally published electronically on the publisher’s internet portal on 7 of March 2020 without open access.With the author(s)’decision to opt for Open Choice,the copyright of the article changed on 11 of April 2020 to©The Author(s),2020 and the article is forthwith distributed under a Creative Commons Attribution 4.0 International License,which permits use,sharing,adaptation,distribution and reproduction in any medium or format,as long as you give appropriate credit to the original author(s)and the source,provide a link to the Creative Commons licence,and indicate if changes were made.The images or other third party material in this article are included in the article’s Creative Commons licence,unless indicated otherwise in a credit line to the material.If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use,you will need to obtain permission directly from the copyright holder.To view a copy of this licence,visit http://creativecommons.org/licenses/by/4.0. | Yan XIA Yongyun HU Jiping LIU Yi HUANG Fei XIE Jintai LIN | 2022 | Advances in Atmospheric Sciences2022，39，9： | 0 |
| 18 | Advances in the Researches of the Middle and Upper Atmosphere in China in 2020-2022显示文摘This report reviews the researches for the middle and upper atmosphere in 2020-2022 by Chinese scientists.The report consists of five parts introducing primarily the results from the aspects of the development of infrastructure,the structure and composition,the climate and modeling,the dynamics for the middle and upper atmosphere,and Coupling between Stratosphere and Troposphere,respectively. | CHEN Zeyu XU Jiyao CHEN Hongbin CHEN Wen REN Rongcai HU Xiong ZHU Yajun XUE Xianghui LU Gaopeng ZHANG Shaodong HUANG Kaiming TIAN Wenshou ZHANG Jiankai HU Dingzhu RAO Jian HU Yongyun XIA Yan | 2022 | 空间科学学报2022，42，4： | 0 |
| 19 | Milankovitch theory and monsoon显示文摘The widely accepted“Milankovitch theory”explains insolation-induced waxing and waning of the ice sheets and their effect on the global climate on orbital timescales.In the past half century,however,the theory has often come under scrutiny,especially regarding its“100-ka problem.”Another drawback,but the one that has received less attention,is the“monsoon problem,”which pertains to the exclusion of monsoon dynamics in classic Milankovitch theory even though the monsoon prevails over the vast low-latitude(30N to30S)region that covers half of the Earth’s surface and receives the bulk of solar radiation.In this review,we discuss the major issues with the current form of Milankovitch theory and the progress made at the research forefront. | Hai Cheng Hanying Li Lijuan Sha Ashish Sinha Zhengguo Shi Qiuzhen Yin Zhengyao Lu Debo Zhao Yanjun Cai Yongyun Hu Qingzhen Hao Jun Tian Gayatri Kathayat Xiyu Dong Jingyao Zhao Haiwei Zhang | 2022 | The Innovation2022，3，6： | 0 |
| 20 | Advances in the Researches of the Middle and Upper Atmosphere in China显示文摘In this paper we summarize the research results by Chinese scientists in 2016–2018. The focuses are placed on the researches of the middle and upper atmosphere, specifically the researches associated with groundbased observation capability development, dynamical processes, and properties of circulation and chemistryclimate coupling of the middle atmospheric layers. | CHEN Zeyu CHEN Hongbin XU Jiyao L Daren ZHANG Shaodong XUE Xianghui TIAN Wenshou LIU Renqiang CHEN Wen HU Yongyun WANG Rui HU Dingzhu HU Xiong YANG Guotao GONG Yun LU Gaopeng | 2018 | 空间科学学报2018，38，5： | 0 |
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