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Observing the air-sea turbulent heat flux on the trajectory of tropical storm Danas

Journal of Oceanology and Limnology 2024年第5期42卷 1425-1437页

作者： Xuehan XIE xiangzhou song.m.rilena oltmanns Yangang LI Qifeng QIAN Zexun WEI Key Laboratory of marine Hazards Forecasting Ministry of Natural ResourcesHohai UniversityNanjing 210098China College of Oceanography Hohai UniversityNanjing 210098China National Oceanography Centre Southampton SO 143 ZHUnited Kingdom East China Sea Forecasting and Disaster Reduction Center Ministry of Natural ResourcesShanghai 200136China National meteorological Centre China Meteorological AdministrationBeijing 100081China First Institute of Oceanography Ministry of Natural ResourcesQingdao 266061China

Tropical cyclones constitute a major risk for coastal *** assess their damage potential,accurate predictions of their intensification are needed,which requires a detailed understanding of the evolution of turbulent heat flux(THF).By combining multiple buoy observations along the south north storm track,we investigated the THF anomalies associated with tropical storm Danas(2019)in the East China Sea(ECS)during its complete life cycle from the intensification stage to the mature stage and finally to its dissipation on *** storm passage is characterized by strong winds of 10-20 m/s and a sea level pressure below 1000 hPa,resulting in a substantial enhancement of *** heat(LH)fluxes are most strongly affected by wind speed,with a gradually increasing contribution of humidity along the *** relative contributions of wind speed and temperature anomalies to sensible heat(SH)depend on the stability of the boundary *** stable conditions,SH variations are driven by wind speed,while under near-neutral conditions,SH variations are driven by temperature.A comparison of the observed THF and associated variables with outputs from the ERA 5 and mERRA 2 reanalysis products reveals that the reanalysis products can reproduce the basic evolution and composition of the observed ***,under extreme weather conditions,temperature and humidity variations are poorly captured by ERA 5 and mERRA 2,leading to large LH and SH *** differences in the observed and reproduced LH and SH during the passage of Danas amount to 26.1 and 6.6 W/m^(2) for ERA 5,respectively,and to 39.4 and 12.5 W/m^(2) for mERRA 2,*** results demonstrate the need to improve the representation of tropical cyclones in reanalysis products to better predict their intensification process and reduce their damage.

关键词： tropical cyclone(TC) air-sea turbulent heat flux(THF) latent heat flux sensible heat flux buoy observation reanalysis product

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New Record Ocean Temperatures and Related Climate Indicators in 2023

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Advances in Atmospheric Sciences 2024年第6期41卷 1068-1082页

作者： Lijing CHENG John ABRAHAm Kevin E.TRENBERTH Tim BOYER michael EmANN Jiang ZHU Fan WANG Fujiang YU Ricardo LOCARNINI John FASULLO Fei ZHENG Yuanlong LI Bin ZHANG Liying WAN Xingrong CHEN Dakui WANG Licheng FENG xiangzhou song Yulong LIU Franco RESEGHETTI Simona SImONCELLI Viktor GOURETSKI Gengxin CHEN Alexey mISHONOV Jim REAGAN Karina VON SCHUCKmANN Yuying PAN Zhetao TAN Yujing ZHU Wangxu WEI Guancheng LI Qiuping REN Lijuan CAO Yayang LU International Center for Climate and Environment Sciences Institute of Atmospheric PhysicsChinese Academy of SciencesBeijing 100029China University of St.Thomas School of EngineeringMinnesota 55105USA NSF National Center for Atmospheric Research BoulderColorado 80307USA University of Auckland Auckland 1010New Zealand National Oceanic and Atmospheric Administration National Centers for Environmental InformationSilver SpringMaryland 20910USA Department of Earth and Environmental Science University of PennsylvaniaPhiladelphiaPennsylvania 19104USA Institute of Oceanology Chinese Academy of SciencesQingdao 266071China National marine Environmental Forecasting Center Ministry of Natural Resources of ChinaBeijing 100081China Oceanographic Data Center Chinese Academy of SciencesQingdao 266071China College of Oceanography Hohai UniversityNanjing 210098China National marine Data and Information Service Tianjin 300171China Italian National Agency for New Technologies Energy and Sustainable Economic DevelopmentS.Teresa Research CenterLerici 19032Italy Istituto Nazionale di Geofisica e Vulcanologia Sede di BolognaBologna 40128Italy South China Sea Institute of Oceanology Chinese Academy of SciencesGuangzhou 510301China ESSIC/CISESS-mD University of MarylandCollege ParkMD20740USA mercator Ocean International Toulouse 31400France Eco-Environmental monitoring and Research Center Pearl River Valley and South China Sea Ecology and Environment AdministrationMinistry of Ecology and EnvironmentPRCGuangzhou 510611China National meteorological Information Center China Meteorological AdministrationBeijing 100081China International Research Center of Big Data for Sustainable Development Goals Beijing 100094China

The global physical and biogeochemical environment has been substantially altered in response to increased atmospheric greenhouse gases from human *** 2023,the sea surface temperature(SST)and upper 2000 m ocean heat content(OHC)reached record *** 0–2000 m OHC in 2023 exceeded that of 2022 by 15±10 ZJ(1 Zetta Joules=1021 Joules)(updated IAP/CAS data);9±5 ZJ(NCEI/NOAA data).The Tropical Atlantic Ocean,the mediterranean Sea,and southern oceans recorded their highest OHC observed since the *** with the onset of a strong El Niño,the global SST reached its record high in 2023 with an annual mean of~0.23℃ higher than 2022 and an astounding>0.3℃ above 2022 values for the second half of *** density stratification and spatial temperature inhomogeneity indexes reached their highest values in 2023.

关键词： ocean heat content salinity stratification global warming climate

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海洋热浪背景下海气湍流热通量资料的评估——以2019年东北太平洋“Blob 2.0”事件为例

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海洋预报 2024年第3期41卷 1-11页

作者：马婧宋翔洲闫运伟王斌陈陟河海大学海洋学院江苏南京210024 自然资源部国家海洋技术中心天津300112 国家海洋环境预报中心北京100081

2019年夏季,东北太平洋地区经历了一次名为“Blob 2.0”的海洋热浪事件,对海洋生态系统造成了严重影响。利用美国国家数据浮标中心的浮标观测资料、全球客观分析通量产品OAFlux,以及大气再分析数据集ERA5、NCEP2和mERRA-2,综合分析了“B... 详细信息

2019年夏季,东北太平洋地区经历了一次名为“Blob 2.0”的海洋热浪事件,对海洋生态系统造成了严重影响。利用美国国家数据浮标中心的浮标观测资料、全球客观分析通量产品OAFlux,以及大气再分析数据集ERA5、NCEP2和mERRA-2,综合分析了“Blob 2.0”事件期间海气湍流热通量的特征,并研究了其物理因素。浮标观测显示,在“Blob 2.0”事件期间,潜热通量呈现正增长趋势,而感热通量呈现负增长趋势,这一现象可归因于海气比湿度差呈正增长,而风速和海气温差呈负增长。评估结果表明:4种通量数据产品都低估了潜热通量的增长,ERA5的增长率与浮标最为接近。对于感热通量,mERRA-2和NCEP2产品的增长趋势与浮标观测相同,其中mERRA-2的增长率更接近;而OAFlux和ERA5产品的增长趋势与观测相反。

关键词：海洋热浪湍流热通量异常浮标观测通量数据集

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Tides and Turbulent mixing in the North of Taiwan Island

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Advances in Atmospheric Sciences 2019年第3期36卷 313-325,341页

作者： xiangzhou song Dexing WU Xiaohui XIE State Oceanic Administration Ministry of Nat-ural Resources Physical Oceanography Laboratory Ocean University of China National marine Environmental Forecasting Center State Oceanic Administration Horn Point Laboratory University of Maryland Center for Environmental Science

microstructure and hydrological profiles were collected along two cross-shelf sections from the deep slope to the shallow water in the north of Taiwan Island in the summer of *** the tidal currents on the shelf were dominated by the barotropic tide with the current ellipse stretched across the shelf,significant internal tides were observed on the *** depth-mean turbulent kinetic energy(TKE)dissipation rate on the shelf was 10^-6W kg^-1,corresponding to a diapycnal diffusivity of 10^-2 m^2s^-*** depth-mean TKE dissipation rate on the slope was 1×10^-7 Wkg^-1,with diapycnal diffusivity of 3×10^-4m^2s^-*** shear instability associated with internal tides largely contributed to the TKE dissipation rate on the slope from the surface to 150 m,while the enhanced turbulence on the shelf was dominated by tidal or residual current dissipations caused by friction in the thick bottom boundary layer(BBL).In the BBL,the Ekman currents associated with the northeastward Taiwan Warm Current were identified,showing a near-bottom velocity spiral,which agreed well with the analytical bottom Ekman solution.

关键词： microstructure observations turbulent mixing internal tides bottom boundary layer bottom Ekman spiral

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A comparison of multiplatform wind products in the South China Sea during summer and autumn in 2019

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Journal of Oceanology and Limnology 2021年第6期39卷 2181-2194页

作者： Yuxin LIU mingsen LIN Xingwei JIANG Xiujun SUN xiangzhou song Key Laboratory of marine Hazards Forecasting Ministry of Natural ResourcesHohai UniversityNanjing 210098China National Satellite Ocean Application Service Beijing 100081China Key Laboratory of Space Ocean Remote Sensing and Application Ministry of Natural ResourcesBeijing 100081China Physical Oceanography Laboratory Ocean University of ChinaQingdao 266100China College of Oceanography Hohai UniversityNanjing 210098China

Sea surface wind(SSW)observations from a newly developed“Black Pearl”wave glider,the Chinese-French Oceanography Satellite(CFOSAT),the HY-2A microwave scatterometer,and a recently released high-resolution atmospheric reanalysis(ERA5)are evaluated with respect to in-situ buoy observations(115.46°E,19.85°N)from the South China *** observations from June to November 2019 are used to evaluate the wind estimates from the different *** comparisons show that the HY-2A and CFOSAT scatterometer wind speeds have mean root mean square errors(RmSEs)of approximately 1.6 and 1.6 m/s,respectively,and the corresponding mean wind direction RmSEs are approximately 19°and 17°,which indicates that these satellite retrievals meet the requirements of design engineering *** wind speed and wind direction RmSEs of ERA5 are approximately 1.9 m/s and 33°,*** correlation coefficients between the HY-2A,CFOSAT,and ERA5 wind speeds and the buoy observations are 0.86,0.85,and 0.84,respectively,and the corresponding coefficients of the wind direction are 0.98,0.98,and 0.93,respectively,at a 95%confidence ***,the wind sensor in the wave glider provides relatively poor-quality observations compared with the buoy measurements and has higher wind speed and wind direction RmSEs of 2.9 m/s and 50.1°,*** diagrams are utilized to illustrate comprehensive wind comparisons between the multiplatform observations and buoy *** results help identify the basic biases in SSWs among different products and enhance confidence in the future use of SSW data for studies of upper ocean dynamics and climate *** are also off ered to help improve the design of next-generation wave gliders.

关键词： sea surface wind(SSW) calibration South China Sea(SCS) wave glider fi fth European Centre for medium-Range Weather Forecasts reanalysis(ERA5) HY-2A Chinese-French Oceanography Satellite(CFOSAT)

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Geostrophic Spirals Generated by the Horizontal Diffusion of Vortex Stretching in the Yellow Sea

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Advances in Atmospheric Sciences 2019年第2期36卷 219-230页

作者： xiangzhou song Rui Xin HUANG Dexing WU Fangli QIAO Guansuo WANG Physical Oceanography Laboratory Ocean University of China State Oceanic Administration Ministry of Natural Resources Department of Physical Oceanography Woods Hole Oceanographic Institution First Institute of Oceanography State Oceanic Administration

Horizontal velocity spirals with a clockwise rotation(downward looking) rate of 1.7?m^(-1), on average, were observed in the western and northern Yellow Sea from December 2006 to February 2007. With the observed thermal wind relation,the beta-spiral theory was used to explain the dynamics of spirals. It was found that the horizontal diffusion of geostrophic vortex stretching is likely to be a major mechanism for generating geostrophic spirals. Vertical advection associated with surface/bottom Ekman pumping and topography-induced upwelling is too weak to support these spirals. Strong wind stirring and large heat loss in wintertime lead to weak stratification and diminish the effects of vertical advection. The cooling effect and vertical diffusion are offset by an overwhelming contribution of horizontal diffusion in connection with vortex stretching. The Richardson number-dependent vertical eddy diffusivity reaches a magnitude of 10^(-4) m^2 s^(-1) on average. An eddy diffusivity of 2870 m^2 s^(-1) is required for dynamic balance by estimating the residual term. This obtained value of 10-4 m^2 s^(-1) is in good agreement with the estimation in terms of observed eddy activities. The suppressed and unsuppressed diffusivities in the observation region are 2752 and 2881 m^2 s^(-1), respectively, which supports a closed budget for velocity rotation.

关键词： geostrophic spirals horizontal diffusion vortex stretching and surface cooling effect

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比例减压阀控缸输出力的非线性自适应控制

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北京理工大学学报 2024年第10期44卷 1066-1076页

作者：王向周韩谦张宁宁郑戍华北京理工大学自动化学院北京100081

针对所研制的一款采用双直动式三通比例减压阀控非对称液压缸驱动的刮板型输送带清扫器进行研究,提出了一种基于PI(Prandtl-Ishlinskii)逆模型前馈补偿的自适应控制算法,改善了比例减压阀固有的压力滞环、死区、增益等非线性,保证了清... 详细信息

针对所研制的一款采用双直动式三通比例减压阀控非对称液压缸驱动的刮板型输送带清扫器进行研究,提出了一种基于PI(Prandtl-Ishlinskii)逆模型前馈补偿的自适应控制算法,改善了比例减压阀固有的压力滞环、死区、增益等非线性,保证了清扫器刮板驱动扭矩的精度,实现了以恒定扭矩在刮板全寿命周期内的高效清洁.针对比例减压阀的滞环特性,采用带遗忘因子的递推最小二乘法在线辨识比例减压阀的PI模型参数,进而求解其逆模型作为线性自抗扰控制器的前馈补偿.仿真和实验结果表明,所提算法有效减小了比例减压阀的滞环、死区和增益等非线性,改善了比例减压阀控缸的动态响应,相较于PID算法,跟踪速度提升了65%,在100~700N·m范围内刮板驱动扭矩误差可控制在±2N·m以内.

关键词：比例减压阀清扫器非线性 PI模型自适应控制

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次氯酸钠强化赤铜矿硫化浮选的影响及机理

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金属矿山 2024年第2期 157-162页

作者：马英强于翔州罗进宋振国印万忠饶峰福州大学紫金地质与矿业学院福建福州350108 矿物加工科学与技术国家重点实验室北京102628 福建省新能源金属绿色提取与高值利用重点实验室福建福州350108

表面适度氧化可以提高赤铜矿硫化浮选的效果。通过纯矿物浮选试验,探究了次氯酸钠对赤铜矿硫化浮选的影响,并采用X射线光电子能谱分析、矿物表面Zeta电位测定等方法,探讨了次氯酸钠强化赤铜矿浮选行为的机理。结果表明:与直接硫化浮选相... 详细信息

表面适度氧化可以提高赤铜矿硫化浮选的效果。通过纯矿物浮选试验,探究了次氯酸钠对赤铜矿硫化浮选的影响,并采用X射线光电子能谱分析、矿物表面Zeta电位测定等方法,探讨了次氯酸钠强化赤铜矿浮选行为的机理。结果表明:与直接硫化浮选相比,次氯酸钠能使赤铜矿的硫化浮选回收率增加8.95个百分点;次氯酸钠能够促进赤铜矿表面的Cu(Ⅰ)组分转变为Cu(Ⅱ)组分,可以增强铜组分与硫化剂的反应活性,强化赤铜矿的硫化效果,对赤铜矿的硫化浮选具有促进作用。

关键词：赤铜矿硫化浮选氧化剂强化硫化表面吸附

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Color tunable and white light emitting via energy transfer in single-phase BiOCl:Er^(3+),Sm^(3+) phosphors for WLEDs

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Journal of Rare Earths 2018年第3期36卷 231-237页

作者： xiangzhou Zhang Yongjin Li Rui Hu Zuyuan Xu Jianbei Qiu Zhengwen Yang Zhiguo song School of materials Science and Engineering Kunming University of Science and Technology School of materials Science and Engineering Sun Yat-sen University

BiOCl crystal shows potential as efficient optical host due to its special layered structure. Here,the luminescence properties of the Er^3＋/Sm^3＋ co-doped BiOCl phosphors as single-phase phosphors were reported. Upon near ultraviolet excitation（NUV, 380 nm corresponding the ^4 I15/2→ ^4 G11/2 transition of Er^3＋ ions）, the phosphors exhibit the efficient characteristic emissions of Er^3＋ and Sm^3＋ ions simultaneously. The energy transfer（ET） from Er^3＋ to Sm^3＋ ions in the layered crystals has been validated by the variation of emission intensities and decay lifetimes respectively, which is ascribed to be a dipoledipole interaction. By virtue of the ET behavior and increasing Sm^3＋ ion concentration, the enhancing emission intensity of Sm^3＋ and the tunability of emission color from yellowish-green（0.318, 0.420） to white（0.343, 0.347） are realized. The results of our work indicate that the Er^3＋/Sm^3＋ co-doped BiOCI phosphor has a promising application serving as single component white emitting phosphors for NUV excited WLEDs.

关键词： BiOCl Er^3+ Sm^3+ Color tunable Photoluminescence Energy transfer

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长江上游典型丘陵山区坡耕地径流及氮磷碳流失特征

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环境工程技术学报 2024年第5期14卷 1589-1598页

作者：王祥陈炜黄国鲜童思陈徐向舟聂玉玺宋永会中国环境科学研究院重庆交通大学河海学院重庆文理学院化学与环境工程学院大连理工大学水利工程学院中国市政工程华北设计研究总院有限公司

持续的坡面降雨可能引发地表径流和壤中流的形成。其中,地表径流可通过溶蚀、侵蚀、运输等方式将大量富集在表土(通常为0~20 mm厚度)的养分从土壤中转移到受纳环境。降雨强度和坡度的变化可以影响坡面径流强度,从而改变径流中总氮(TN)... 详细信息

持续的坡面降雨可能引发地表径流和壤中流的形成。其中,地表径流可通过溶蚀、侵蚀、运输等方式将大量富集在表土(通常为0~20 mm厚度)的养分从土壤中转移到受纳环境。降雨强度和坡度的变化可以影响坡面径流强度,从而改变径流中总氮(TN)、总磷(TP)、溶解性有机碳(DOC)等养分浓度与通量过程。通过模拟降雨试验,设置3种典型降雨强度(40、60、90mm/h)和坡度(6°、12°、18°),探讨不同条件下丘陵山区紫色土坡面径流及坡面TN、TP、DOC流失特征。结果表明:1)产流临界坡度不是一个定值,降雨强度在60 mm/h及以下时,临界坡度介于6°~18°;降雨强度达到90 mm/h时,未出现明显的临界坡度。2)相同降雨强度下,径流中TN和DOC浓度与坡度呈正相关(18°>12°>6°);降雨强度为90 mm/h时,径流中TP浓度与坡度的关系为6°>12°>18°,其余降雨强度下,则为12°>18°>6°。除12°坡面外,DOC流失量随降雨强度增加呈上升趋势;TP最大流失量出现在90 mm/h降雨强度下的6°坡面,为0.91 mg/m^(2),表现为来源限制,其余坡度坡面的TP流失表现为携带限制。3)坡面产流量和产沙量主要受降雨强度的影响,产流量和降雨强度与径流中TP流失量和DOC流失量显著相关,坡度与碳、氮、磷流失量的相关性均不显著,径流中TN流失量与TP和DOC流失量显著相关。研究显示,高强度降雨和小坡度组合下,径流量、TP流失量、DOC流失量显著高于其余降雨强度和坡度的组合,而在高强度降雨和大坡度组合下,TN流失量达到峰值。因此,需要特别关注强降雨、小坡度下紫色土中TP、DOC流失及强降雨、大坡度下TN流失问题。

关键词：紫色土降雨强度坡度模拟降雨养分流失

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