At present,the identification of tropical cyclone remote precipitation(TRP)requires subjective participation,leading to inconsistent results among different researchers despite adopting the same identification standar...At present,the identification of tropical cyclone remote precipitation(TRP)requires subjective participation,leading to inconsistent results among different researchers despite adopting the same identification standard.Thus,establishing an objective identification method is greatly important.In this study,an objective synoptic analysis technique for TRP(OSAT_TRP)is proposed to identify TRP using daily precipitation datasets,historical tropical cyclone(TC)track data,and the ERA5 reanalysis data.This method includes three steps:first,independent rain belts are separated,and those that might relate to TCs'remote effects are distinguished according to their distance from the TCs.Second,the strong water vapor transport belt from the TC is identified using integrated horizontal water vapor transport(IVT).Third,TRP is distinguished by connecting the first two steps.The TRP obtained through this method can satisfy three criteria,as follows:1)the precipitation occurs outside the circulation of TCs,2)the precipitation is affected by TCs,and 3)a gap exists between the TRP and TC rain belt.Case diagnosis analysis,compared with subjective TRP results and backward trajectory analyses using HYSPLIT,indicates that OSAT_TRP can distinguish TRP even when multiple TCs in the Northwest Pacific are involved.Then,we applied the OSAT_TRP to select typical TRPs and obtained the synoptic-scale environments of the TRP through composite analysis.展开更多
Objective:To evaluate how DNA fragmentation index(DFI)and chromatin denaturation index(CDI)relate to semen parameters across different types of male infertility,thereby improving the understanding and assessment of sp...Objective:To evaluate how DNA fragmentation index(DFI)and chromatin denaturation index(CDI)relate to semen parameters across different types of male infertility,thereby improving the understanding and assessment of sperm quality.Methods:A prospective and descriptive cohort study was conducted over two years at the Integrated Physiology Laboratory of the University of Carthage in collaboration with the Alyssa Fertility Group,Tunisia.A total of 163 participants were classified into five groups based on their semen parameters:normozoospermia,oligozoospermia,asthenozoospermia,teratozoospermia,and oligoastheno-teratozoospermia.The normozoospermia group was selected from volunteers who had children.Semen samples were analyzed according to WHO guidelines.DFI was measured using Halosperm®and CDI was tested using aniline blue staining.Results:Both DFI and CDI were significantly higher in all infertility groups,with the oligozoospermia group showing the highest DFI and CDI.Negative correlations were found between DFI/CDI and sperm motility,concentration,and morphology in the affected groups.The normozoospermia group served as a control with the lowest DFI and CDI values.Conclusions:DFI and CDI are increasingly recognized as important biomarkers for evaluating sperm quality in cases of male infertility.Their elevated levels in patients with oligozoospermia,asthenozoospermia,teratozoospermia,and oligo-asthenoteratozoospermia underscore their potential role in not only diagnosing male infertility but also in assessing the overall reproductive outcomes for affected individuals,thus guiding more effective treatment strategies.展开更多
利用NCEP/NCAR(美国国家环境预报中心/国家大气研究中心)的全球预报系统(GFS)再分析资料、欧洲气象中心(ERA-interim)资料以及中国气象局观测站点的实况降水观测结合CMORPH卫星反演降水资料,对2014年第10号台风Matmo生成后西北行并登陆...利用NCEP/NCAR(美国国家环境预报中心/国家大气研究中心)的全球预报系统(GFS)再分析资料、欧洲气象中心(ERA-interim)资料以及中国气象局观测站点的实况降水观测结合CMORPH卫星反演降水资料,对2014年第10号台风Matmo生成后西北行并登陆台湾及福建过程中的特征进行了分析,揭示出Matmo移动路径主要受西太平洋副热带高压(简称西太副高)外围引导气流影响。动、热力物理量场分析表明,Matmo在登陆福建前后,福建上空一直维持深厚的涡旋结构,福建东南部上空的上升区与台湾海峡及福建西部附近的下沉运动区形成明显的垂直环流圈。同时,南海上空有明显的西南急流(风速大于16 m s^(-1)),Matmo的水汽来源主要有两条,分别为孟加拉湾和南海以及西太副高南侧。充足的水汽输送及低层水汽辐合抬升有利于Matmo登陆后的强降水发生和维持。Matmo登陆福建后仍然保持低层辐合、高层辐散,有利于持续暴雨的发生。Matmo登陆福建期间始终处于风速垂直切变小值区(小于9 m s^(-1))中,环境风速的弱垂直切变有利于Matmo暖心结构及高空辐散形势的维持,是Matmo在登陆后依然能维持自身强度不衰减的原因之一。展开更多
针对2008年初发生在贵州地区的严重冻雨过程,分别从环流背景、低空急流和水汽输送条件等方面分析了准静止锋维持的原因,并选取本次灾害最严重的第3次过程为典型个例,利用WRF模式针对准静止锋影响下的贵州冻雨进行数值模拟来研究冻雨的...针对2008年初发生在贵州地区的严重冻雨过程,分别从环流背景、低空急流和水汽输送条件等方面分析了准静止锋维持的原因,并选取本次灾害最严重的第3次过程为典型个例,利用WRF模式针对准静止锋影响下的贵州冻雨进行数值模拟来研究冻雨的发生机制。模拟结果较好地反映出高低空环流形势场特征,强雨雪降水带的走向、落区,以及地面温度的分布,均与观测基本吻合。通过分析高分辨率模式的模拟结果,揭示了准静止锋上贵州地区冻雨的层结结构特征及云物质在冻雨区的分布特征。研究结果表明,贵州中部的冻雨区除一般的三层结构(包含冰晶层、暖层和冷层)外,还具有典型的两层结构特征,即:高空的固体降水粒子稀少,900~600 h Pa深厚的逆温层和0℃以上的暖层使中低空存在大量液态粒子,下落的液滴经过近地面的浅薄冷层,形成大量过冷却雨滴,而后降落至地面迅速冻结。展开更多
基金supported by the Postgraduate Research&Practice Innovation Program of Jiangsu Province(No.KYCX22_1136)the National Natural Scientific Foundation of China(No.42275037)+2 种基金the Basic Research Fund of CAMS(No.2023Z016)the Key Laboratory of South China Sea Meteorological Disaster Prevention and Mitigation of Hainan Province(No.SCSF202202)supported by the Jiangsu Collaborative Innovation Center for Climate Change。
文摘At present,the identification of tropical cyclone remote precipitation(TRP)requires subjective participation,leading to inconsistent results among different researchers despite adopting the same identification standard.Thus,establishing an objective identification method is greatly important.In this study,an objective synoptic analysis technique for TRP(OSAT_TRP)is proposed to identify TRP using daily precipitation datasets,historical tropical cyclone(TC)track data,and the ERA5 reanalysis data.This method includes three steps:first,independent rain belts are separated,and those that might relate to TCs'remote effects are distinguished according to their distance from the TCs.Second,the strong water vapor transport belt from the TC is identified using integrated horizontal water vapor transport(IVT).Third,TRP is distinguished by connecting the first two steps.The TRP obtained through this method can satisfy three criteria,as follows:1)the precipitation occurs outside the circulation of TCs,2)the precipitation is affected by TCs,and 3)a gap exists between the TRP and TC rain belt.Case diagnosis analysis,compared with subjective TRP results and backward trajectory analyses using HYSPLIT,indicates that OSAT_TRP can distinguish TRP even when multiple TCs in the Northwest Pacific are involved.Then,we applied the OSAT_TRP to select typical TRPs and obtained the synoptic-scale environments of the TRP through composite analysis.
文摘Objective:To evaluate how DNA fragmentation index(DFI)and chromatin denaturation index(CDI)relate to semen parameters across different types of male infertility,thereby improving the understanding and assessment of sperm quality.Methods:A prospective and descriptive cohort study was conducted over two years at the Integrated Physiology Laboratory of the University of Carthage in collaboration with the Alyssa Fertility Group,Tunisia.A total of 163 participants were classified into five groups based on their semen parameters:normozoospermia,oligozoospermia,asthenozoospermia,teratozoospermia,and oligoastheno-teratozoospermia.The normozoospermia group was selected from volunteers who had children.Semen samples were analyzed according to WHO guidelines.DFI was measured using Halosperm®and CDI was tested using aniline blue staining.Results:Both DFI and CDI were significantly higher in all infertility groups,with the oligozoospermia group showing the highest DFI and CDI.Negative correlations were found between DFI/CDI and sperm motility,concentration,and morphology in the affected groups.The normozoospermia group served as a control with the lowest DFI and CDI values.Conclusions:DFI and CDI are increasingly recognized as important biomarkers for evaluating sperm quality in cases of male infertility.Their elevated levels in patients with oligozoospermia,asthenozoospermia,teratozoospermia,and oligo-asthenoteratozoospermia underscore their potential role in not only diagnosing male infertility but also in assessing the overall reproductive outcomes for affected individuals,thus guiding more effective treatment strategies.
文摘利用NCEP/NCAR(美国国家环境预报中心/国家大气研究中心)的全球预报系统(GFS)再分析资料、欧洲气象中心(ERA-interim)资料以及中国气象局观测站点的实况降水观测结合CMORPH卫星反演降水资料,对2014年第10号台风Matmo生成后西北行并登陆台湾及福建过程中的特征进行了分析,揭示出Matmo移动路径主要受西太平洋副热带高压(简称西太副高)外围引导气流影响。动、热力物理量场分析表明,Matmo在登陆福建前后,福建上空一直维持深厚的涡旋结构,福建东南部上空的上升区与台湾海峡及福建西部附近的下沉运动区形成明显的垂直环流圈。同时,南海上空有明显的西南急流(风速大于16 m s^(-1)),Matmo的水汽来源主要有两条,分别为孟加拉湾和南海以及西太副高南侧。充足的水汽输送及低层水汽辐合抬升有利于Matmo登陆后的强降水发生和维持。Matmo登陆福建后仍然保持低层辐合、高层辐散,有利于持续暴雨的发生。Matmo登陆福建期间始终处于风速垂直切变小值区(小于9 m s^(-1))中,环境风速的弱垂直切变有利于Matmo暖心结构及高空辐散形势的维持,是Matmo在登陆后依然能维持自身强度不衰减的原因之一。
文摘针对2008年初发生在贵州地区的严重冻雨过程,分别从环流背景、低空急流和水汽输送条件等方面分析了准静止锋维持的原因,并选取本次灾害最严重的第3次过程为典型个例,利用WRF模式针对准静止锋影响下的贵州冻雨进行数值模拟来研究冻雨的发生机制。模拟结果较好地反映出高低空环流形势场特征,强雨雪降水带的走向、落区,以及地面温度的分布,均与观测基本吻合。通过分析高分辨率模式的模拟结果,揭示了准静止锋上贵州地区冻雨的层结结构特征及云物质在冻雨区的分布特征。研究结果表明,贵州中部的冻雨区除一般的三层结构(包含冰晶层、暖层和冷层)外,还具有典型的两层结构特征,即:高空的固体降水粒子稀少,900~600 h Pa深厚的逆温层和0℃以上的暖层使中低空存在大量液态粒子,下落的液滴经过近地面的浅薄冷层,形成大量过冷却雨滴,而后降落至地面迅速冻结。
