To investigate the impacts of solar radiation on tropical cyclone （TC） warm-core structure （i.e., the magnitude and height）, a pair of idealized simulations are conducted by specifying different strengths of solar...To investigate the impacts of solar radiation on tropical cyclone （TC） warm-core structure （i.e., the magnitude and height）, a pair of idealized simulations are conducted by specifying different strengths of solar shortwave radiation. It is found that the TC warm core is highly sensitive to the shortwave radiative effect. For the nighttime storm, a tendency for a more intense warm core is found, with an elevated height compared to its daytime counterpart. As pointed out by previous studies, the radiative cooling during nighttime destabilizes the local and large-scale environment and thus promotes deep moist convec- tion, which enhances the TC＇s intensity. Due to the different inertial stabilities, the diabatic heating in the eyewall will force different secondary circulations. For a strong TC with a deeper vertical structure, this promotes a thin upper-level inflow layer. This inflow carries the lower stratospheric air with high potential temperature and descends adiabatically in the eye, resulting in significant upper-level warming. The Sawyer-Eliassen diagnosis further confirms that the height of the maximum temperature anomaly is likely attributable to the balance among the forced secondary circulations.展开更多
Through a cloud-resolving simulation of the rapid intensification(RI)of Typhoon Meranti(2016),the convections,warm core,and heating budget are investigated during the process of RI.By investigating the spatial distrib...Through a cloud-resolving simulation of the rapid intensification(RI)of Typhoon Meranti(2016),the convections,warm core,and heating budget are investigated during the process of RI.By investigating the spatial distributions and temporal evolutions of both convectivestratiform precipitation and shallow-deep convections,we find that the inner-core convections take mode turns,from stratiform-precipitation(SP)dominance to convectiveprecipitation(CP)prevalence during the transition stages between pre-RI and RI.For the CP,it experiences fewer convections before RI,and the conversion from moderate/moderate-deep convections to moderate-deep/deep convections during RI.There is a clear upper-level warm-core structure during the process of RI.However,the mid-lowlevel warming begins first,before the RI of Meranti.By calculating the local potential temperature(0)budget of various convections,the link between convections and the warm core(and further to RI via the pressure drop due to the warming core)is established.Also,the transport pathways of heating toward the center of Meranti driven by pressure are illuminated.The total hydrostatic pressure decline is determined by the mid-low-level warm anomaly before RI,mostly caused by SP.The azimuthal-mean diabatic heating is the largest heating source,the mean vertical heat advection controls the vertical downwards transport by adiabatic warming of compensating downdrafts above eye region,and then the radial 6 advection term radially transports heat toward the center of Meranti in a slantwise direction.Accompanying the onset of RI,the heating efficiency of the upper-level warming core rises swiftly and overruns that of the mid-low-level warmanomaly, dominating the total pressure decrease and beingmainly led by moderate-deep and deep convections. Asidefrom the characteristics in common with SP, for CP, theeddy component of radial advection also plays a positiverole in warming the core, which enhances the centripetaltransport effect and accelerates the RI of Meranti.展开更多
The linear regression and horizontally stepwise correction are conducted on the observational data from AMSU-A L1 B of NOAA polar orbit satellite to invert a 40-layers(from 1,000 h Pa to 0.1 h Pa) dataset of atmospher...The linear regression and horizontally stepwise correction are conducted on the observational data from AMSU-A L1 B of NOAA polar orbit satellite to invert a 40-layers(from 1,000 h Pa to 0.1 h Pa) dataset of atmospheric temperature with a horizontal resolution of 0.5°×0.5° after the correction of satellite antenna pattern and limb adjustment. Case study shows that the inversion data of temperature can reveal the detail structure of warm core in tropical cyclone. We choose two categories of tropical depressions(TDs) over the South China Sea, including the non-developing TDs and developing TDs. Both of them are developed downward from the middle and upper level to the lower level. Comparison between the evolutions of warm core in the two categories of TDs indicates that the warm core is developed downward from the middle and upper troposphere to the sea surface in all the downward-developing TDs. The difference is that in the group of further developing TDs, the warm core in the upper troposphere is intensified suddenly when it is extending to the sea surface. The warm core in the upper and lower troposphere is strengthened in a meantime. But the similar feature is not observed in the non-developing TDs. Then it may be helpful to judge the TD development by monitoring the change in its warm-core structure.展开更多
During the boreal spring of 1966, a warm-core eddy is identified in the upper South China Sea (SCS) west of the Philippines through an analysis of the U.S. Navy′s Master Oceanographic Observation Data Set. This eddy ...During the boreal spring of 1966, a warm-core eddy is identified in the upper South China Sea (SCS) west of the Philippines through an analysis of the U.S. Navy′s Master Oceanographic Observation Data Set. This eddy occurred before the development of the northern summer monsoon and disappeared afterward. We propose that this eddy is a result of the radiative warming during spring and the downwelling due to the anticyclonic forcing at the surface. Our hypothesis suggests an air-sea feedback scenario that may explain the development and withdrawal of the summer monsoon over the SCS. The development phase of the warm-core eddy in this hypothesis is tested by using the Princeton Ocean model.展开更多
The warming of Antarctica observed in recent years is one of the consequences of deep degassing associated with the northward drift of the Earth’s core. Ascending streams of hydrogen and other gases move along the te...The warming of Antarctica observed in recent years is one of the consequences of deep degassing associated with the northward drift of the Earth’s core. Ascending streams of hydrogen and other gases move along the tectonic faults of the lithosphere. When they get into an oxidizing environment, there is an increase in the amount of water in the ocean and air, which is accompanied by a decrease in oxygen concentrations and the release of huge amounts of energy. The provisions of the proposed theory were tested using the method of mental critical experiment. The reality of atmospheric effects of subsurface degassing is confirmed by the facts of synchronous destruction of ozone in the stratosphere and an increase in the temperature of the surface air layer. These events usually coincide with releases of ozone-depleting and heat-generating hydrogen from the subsurface.展开更多
目的系统评价身上型和身下全身型充气式保温毯维持腹部手术患者围手术期核心体温的有效性,为腹部手术患者选择合适、有效的主动保温方法提供临床依据。方法通过计算机检索PubMed、Cochrane Library、Web of Science、Scopus、Embase、CI...目的系统评价身上型和身下全身型充气式保温毯维持腹部手术患者围手术期核心体温的有效性,为腹部手术患者选择合适、有效的主动保温方法提供临床依据。方法通过计算机检索PubMed、Cochrane Library、Web of Science、Scopus、Embase、CINAHL、中国知网以及万方数据库,收集身上型和身下全身型充气式保温毯对维持腹部手术患者核心体温有效性的随机对照试验,并追溯其参考文献,检索时限均为建库至2023年3月。2位研究者独立进行文献筛选、数据提取和质量评价后,采用Rev Man 5.4软件对纳入文献进行Meta分析。结果最终纳入5项随机对照试验,总样本量为373例患者。Meta分析结果显示,身下全身型充气式保温毯能升高患者术中核心体温[95%CI为0.13(0.02~0.29),P<0.001],降低围术期非计划低体温的发生率[95%CI为0.15(0.03~0.79),P=0.020],并减少术后寒战的发生[95%CI为0.17(0.05~0.63),P=0.008]。结论身下全身型充气式保温毯对维持腹部手术患者围手术期核心体温有效,可降低围术期非计划低体温和寒战的发生风险。展开更多
利用常规观测资料、FY-2C卫星云图、NCEP/NCAR再分析资料,对一次西南低涡暴雨过程进行了诊断分析。结果表明,这次暴雨天气过程的主要影响系统有对流层高层南亚高压、中层低涡、低层切变线(低涡)以及台风"天鹅"。该过程是由3...利用常规观测资料、FY-2C卫星云图、NCEP/NCAR再分析资料,对一次西南低涡暴雨过程进行了诊断分析。结果表明,这次暴雨天气过程的主要影响系统有对流层高层南亚高压、中层低涡、低层切变线(低涡)以及台风"天鹅"。该过程是由3个接连发生的中尺度对流云团直接造成的,发生在西南低涡闭合涡旋范围内的非对称处。利用WRF_ARW(The Advanced Research WRF)中尺度模式进行了数值模拟,结果表明,对流层高层南亚高压脊线附近的强辐散、对流层中层低涡的垂直涡度耦合和对流层低层强劲的东风干冷急流与南风暖湿急流在四川盆地内交汇,促使西南低涡发展、加强。对流层高层的强辐散和低层强辐合相配合,有利于西南低涡的增强、发展。温度场上,发展的西南低涡在300hPa附近出现"暖心"结构,在850hPa以下北冷南暖,冷暖空气交界随着高度的增加向北倾斜。低涡中心南北两侧的次级环流圈上升支在低涡中心附近汇合,出现剧烈的上升运动,促使西南低涡增强。随着高层南亚高压的南移、高空急流的南压,高层辐散减弱,西南低涡也减弱。当中层西风大槽主体移过河套地区,其携带的强冷空气沿高原东侧迅速南下,大量冷空气进入四川盆地,促使西南低涡向南移出盆地,最终减弱、填塞。展开更多
基金sponsored by the National Key Basic Research Program of China (Grant No. 2015CB452803)the National Natural Science Foundation of China (Grant No. 41275095)+2 种基金the "Six peaks of high-level talent" funding project of Jiangsuthe Key University Science Research Project of Jiangsu Province (Grant No. 14KJA170005)the China Meteorological Administration Henan Key Laboratory of Agrometeorological Support and Applied Technique (Grant No. AMF201403)
文摘To investigate the impacts of solar radiation on tropical cyclone （TC） warm-core structure （i.e., the magnitude and height）, a pair of idealized simulations are conducted by specifying different strengths of solar shortwave radiation. It is found that the TC warm core is highly sensitive to the shortwave radiative effect. For the nighttime storm, a tendency for a more intense warm core is found, with an elevated height compared to its daytime counterpart. As pointed out by previous studies, the radiative cooling during nighttime destabilizes the local and large-scale environment and thus promotes deep moist convec- tion, which enhances the TC＇s intensity. Due to the different inertial stabilities, the diabatic heating in the eyewall will force different secondary circulations. For a strong TC with a deeper vertical structure, this promotes a thin upper-level inflow layer. This inflow carries the lower stratospheric air with high potential temperature and descends adiabatically in the eye, resulting in significant upper-level warming. The Sawyer-Eliassen diagnosis further confirms that the height of the maximum temperature anomaly is likely attributable to the balance among the forced secondary circulations.
基金Very thanks for the valuable comments of the three anonymous reviewers,which helped considerably in improving the original manuscript.This work was supported by the National Key Research and Development Program of China(Grant Nos.2018YFC1506801 and 2018YFF0300102)the Plateau Atmosphere and Environment Key Laboratory of Sichuan Province(Grant No.PAEKL-2017-K3)the National Natural Science Foundation of China(Grant Nos.41405059,41575064,41875079,41875077,41575093,and 41630532).
文摘Through a cloud-resolving simulation of the rapid intensification(RI)of Typhoon Meranti(2016),the convections,warm core,and heating budget are investigated during the process of RI.By investigating the spatial distributions and temporal evolutions of both convectivestratiform precipitation and shallow-deep convections,we find that the inner-core convections take mode turns,from stratiform-precipitation(SP)dominance to convectiveprecipitation(CP)prevalence during the transition stages between pre-RI and RI.For the CP,it experiences fewer convections before RI,and the conversion from moderate/moderate-deep convections to moderate-deep/deep convections during RI.There is a clear upper-level warm-core structure during the process of RI.However,the mid-lowlevel warming begins first,before the RI of Meranti.By calculating the local potential temperature(0)budget of various convections,the link between convections and the warm core(and further to RI via the pressure drop due to the warming core)is established.Also,the transport pathways of heating toward the center of Meranti driven by pressure are illuminated.The total hydrostatic pressure decline is determined by the mid-low-level warm anomaly before RI,mostly caused by SP.The azimuthal-mean diabatic heating is the largest heating source,the mean vertical heat advection controls the vertical downwards transport by adiabatic warming of compensating downdrafts above eye region,and then the radial 6 advection term radially transports heat toward the center of Meranti in a slantwise direction.Accompanying the onset of RI,the heating efficiency of the upper-level warming core rises swiftly and overruns that of the mid-low-level warmanomaly, dominating the total pressure decrease and beingmainly led by moderate-deep and deep convections. Asidefrom the characteristics in common with SP, for CP, theeddy component of radial advection also plays a positiverole in warming the core, which enhances the centripetaltransport effect and accelerates the RI of Meranti.
基金National Natural Science Foundation of China(40875026,91015011)Project for Natural Science Foundation Teams of Guangdong Province(8351030101000002)Specialized Program for Social Welfare Industries(Meteorological Sector)(GYHY201106036)
文摘The linear regression and horizontally stepwise correction are conducted on the observational data from AMSU-A L1 B of NOAA polar orbit satellite to invert a 40-layers(from 1,000 h Pa to 0.1 h Pa) dataset of atmospheric temperature with a horizontal resolution of 0.5°×0.5° after the correction of satellite antenna pattern and limb adjustment. Case study shows that the inversion data of temperature can reveal the detail structure of warm core in tropical cyclone. We choose two categories of tropical depressions(TDs) over the South China Sea, including the non-developing TDs and developing TDs. Both of them are developed downward from the middle and upper level to the lower level. Comparison between the evolutions of warm core in the two categories of TDs indicates that the warm core is developed downward from the middle and upper troposphere to the sea surface in all the downward-developing TDs. The difference is that in the group of further developing TDs, the warm core in the upper troposphere is intensified suddenly when it is extending to the sea surface. The warm core in the upper and lower troposphere is strengthened in a meantime. But the similar feature is not observed in the non-developing TDs. Then it may be helpful to judge the TD development by monitoring the change in its warm-core structure.
文摘During the boreal spring of 1966, a warm-core eddy is identified in the upper South China Sea (SCS) west of the Philippines through an analysis of the U.S. Navy′s Master Oceanographic Observation Data Set. This eddy occurred before the development of the northern summer monsoon and disappeared afterward. We propose that this eddy is a result of the radiative warming during spring and the downwelling due to the anticyclonic forcing at the surface. Our hypothesis suggests an air-sea feedback scenario that may explain the development and withdrawal of the summer monsoon over the SCS. The development phase of the warm-core eddy in this hypothesis is tested by using the Princeton Ocean model.
文摘The warming of Antarctica observed in recent years is one of the consequences of deep degassing associated with the northward drift of the Earth’s core. Ascending streams of hydrogen and other gases move along the tectonic faults of the lithosphere. When they get into an oxidizing environment, there is an increase in the amount of water in the ocean and air, which is accompanied by a decrease in oxygen concentrations and the release of huge amounts of energy. The provisions of the proposed theory were tested using the method of mental critical experiment. The reality of atmospheric effects of subsurface degassing is confirmed by the facts of synchronous destruction of ozone in the stratosphere and an increase in the temperature of the surface air layer. These events usually coincide with releases of ozone-depleting and heat-generating hydrogen from the subsurface.
文摘目的系统评价身上型和身下全身型充气式保温毯维持腹部手术患者围手术期核心体温的有效性,为腹部手术患者选择合适、有效的主动保温方法提供临床依据。方法通过计算机检索PubMed、Cochrane Library、Web of Science、Scopus、Embase、CINAHL、中国知网以及万方数据库,收集身上型和身下全身型充气式保温毯对维持腹部手术患者核心体温有效性的随机对照试验,并追溯其参考文献,检索时限均为建库至2023年3月。2位研究者独立进行文献筛选、数据提取和质量评价后,采用Rev Man 5.4软件对纳入文献进行Meta分析。结果最终纳入5项随机对照试验,总样本量为373例患者。Meta分析结果显示,身下全身型充气式保温毯能升高患者术中核心体温[95%CI为0.13(0.02~0.29),P<0.001],降低围术期非计划低体温的发生率[95%CI为0.15(0.03~0.79),P=0.020],并减少术后寒战的发生[95%CI为0.17(0.05~0.63),P=0.008]。结论身下全身型充气式保温毯对维持腹部手术患者围手术期核心体温有效,可降低围术期非计划低体温和寒战的发生风险。
基金This study was supported by the Hunan Provincial Natural Science Foundation of China[grant number 2021JC0009]the Natural Science Foundation of China[grant number U2142212]the National Key R&D Program of China[grant number 2022YFC3004200].
文摘利用常规观测资料、FY-2C卫星云图、NCEP/NCAR再分析资料,对一次西南低涡暴雨过程进行了诊断分析。结果表明,这次暴雨天气过程的主要影响系统有对流层高层南亚高压、中层低涡、低层切变线(低涡)以及台风"天鹅"。该过程是由3个接连发生的中尺度对流云团直接造成的,发生在西南低涡闭合涡旋范围内的非对称处。利用WRF_ARW(The Advanced Research WRF)中尺度模式进行了数值模拟,结果表明,对流层高层南亚高压脊线附近的强辐散、对流层中层低涡的垂直涡度耦合和对流层低层强劲的东风干冷急流与南风暖湿急流在四川盆地内交汇,促使西南低涡发展、加强。对流层高层的强辐散和低层强辐合相配合,有利于西南低涡的增强、发展。温度场上,发展的西南低涡在300hPa附近出现"暖心"结构,在850hPa以下北冷南暖,冷暖空气交界随着高度的增加向北倾斜。低涡中心南北两侧的次级环流圈上升支在低涡中心附近汇合,出现剧烈的上升运动,促使西南低涡增强。随着高层南亚高压的南移、高空急流的南压,高层辐散减弱,西南低涡也减弱。当中层西风大槽主体移过河套地区,其携带的强冷空气沿高原东侧迅速南下,大量冷空气进入四川盆地,促使西南低涡向南移出盆地,最终减弱、填塞。
