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1.
甘肃河西走廊春季强沙尘暴与低空急流   总被引:20,自引:8,他引:12  
使用NCEP/NCAR全球再分析网格点资料(2.5°×2.5°纬度/经度)和我国区域性沙尘暴过程历史资料,分析了春季大气环流特征及低空急流与甘肃河西走廊春季强沙尘暴的关系。结果表明,在东亚中纬度高空维持纬向强急流锋区的情况下,极易造成甘肃河西走廊春季强沙尘暴的低空急流产生。揭示了沙尘暴形成的大尺度环流动力影响因子的事实,指出可将产生这种低空急流特征的西风带大型环流的调整过程,作为甘肃河西走廊春季强沙尘暴天气的预警信号,而低空急流的位置及强度又可作为沙尘暴强度及沙尘暴发生和影响区的预报指标。  相似文献   

2.
青藏高原东北侧地区干湿年夏季环流异常的对比分析   总被引:5,自引:1,他引:4  
使用NCEP/NCAR1968~1997年6~8月平均再分析全球网格点资料以及同期青藏高原东北侧17站夏季总降水量观测资料,对青藏高原东北侧典型干湿年夏季平均的大尺度环流场和物理量场差异进行了对比分析,探讨了青藏高原东北侧夏季干湿年形成的原因和机制。结果表明,青藏高原东北侧区域干湿年夏季对应的大尺度环流场和有关物理量场差异明显,最后给出了青藏高原东北侧夏季干湿年的物理图像,为短期气候预测提供依据。  相似文献   

3.
赵红岩 《气象》2000,26(2):33-36
选用 1 95 1~ 1 996年中国 1 6 0站逐月降水资料 ,太平洋逐月平均网格点海温资料( 1 0°S~ 5 0°N,1 2 0~ 80°E) ,逐月大尺度环流指数资料 ,分析并探讨造成 1 996年南方洪涝的环流特征、气候背景及海温影响机制。结果表明 :大气环流指数与前期太平洋海温场有明显的遥相关关系。冬、春季海温的冷暖变化程度 ,可预示后期 7月各环流系统的趋势变化 ,环流系统指数自身演变存在较明显的年代际变化规律 ,1 996年南方洪涝就是在这种气候背景下形成的。海温冷暖变化影响大气环流系统的这种演变关系 ,对南方洪涝的短期气候预测具有一定的指示意义。  相似文献   

4.
利用常规气象观测资料、NCEP/NCAR 1°×1° 6 h分析资料和2.5°×2.5°日平均再分析资料、自动雨量站资料,采用统计对比分析、诊断分析等方法,对三门峡市2014年9月7—18日连阴雨过程的环流形势、物理量场进行分析,找出此次连阴雨天气的主要成因,结果表明:1)南亚高压的异常偏北偏强为连阴雨天气提供了有利的大尺度环流背景。2)副热带高压的长时间稳定维持,对减缓低槽和切变线移速、促使暖湿气流向北输送十分有利。3)乌拉尔山高压脊较常年同期偏弱,与常见连阴雨天气乌拉尔山高压脊异常偏强的形势有所不同。4)稳定的副热带高空西风急流与副高外围的西南低空急流耦合,为连阴雨提供了持续的上升运动和水汽辐合。5)强降水的产生只有充足的水汽供给是不够的,还必须在水汽的输送区有明显的水汽辐合。6)低层强烈的垂直上升运动为此次连阴雨期间暴雨的形成提供了有利的动力条件。  相似文献   

5.
利用MICAPS资料、FY-2C红外卫星云图和2.5°×2.5°NCEP再分析资料,对2008年5月25日至28日大范围沙尘暴过程进行了天气动力诊断和物理量场分析。结果表明,强沙尘暴主要出现在冷平流前的温度梯度密集区和涡度梯度密集、陡峭区。在这次强沙尘暴过程中,暖平流是蒙古气旋发生、发展的重要热力因子,大气热力不稳定和强风是起沙的动力;500 hPa阶梯槽快速东移是飚线产生的触发系统;对流风暴是引发强沙尘暴主要因素。蒙古气旋的发展加大了冷锋前后的气压和温度梯度,为对流风暴的发生提供了热力不稳定条件。700 hPa冷平流爆发性下沉、南下,为强沙尘暴的产生提供了强大动力。  相似文献   

6.
利用常规观测资料和NCEP 2.5°×2.5°网格再分析资料,对2009年4月16日天山翻山大风的物理机制进行了诊断分析。结果表明:高空急流、垂直环流共同作用是高空动量下传的重要动力机制,500~850hPa较深厚的强冷平流输送是翻山大风形成的热力因子。同时得到天山翻山大风一些有益的预报指标。  相似文献   

7.
使用NECP/NCAR1958~1997年40年再分析全球月平均网格点资料以及相应时段全国160个代表站月降水量资料,针对青藏高原东北侧1997年发生的严重春末夏初旱和伏旱,分析了这次大旱的天气气候背景和500hPa环流场主要特征,对有关物理量场进行了诊断分析,探讨了该年春夏干旱发生的500hPa环流特征,为短期气候预测提供依据。  相似文献   

8.
越赤道气流通道上的经向垂直环流结构   总被引:1,自引:0,他引:1  
本文运用1981年夏季月份,各标准等压面上格点风资料,分析了东半球低纬地区(40°—180°E、30°N—30°S),越赤道气流通道上各种物理量场分布和经向垂直环流。从而揭示了越亦道气流和季风环流及哈德莱环流相互之间的关系。  相似文献   

9.
青藏高原东北侧初夏干湿年500 hPa环流场特征分析   总被引:13,自引:6,他引:7  
使用NCEP/NCAR1958~1997年40年再分析全球月平均网络点资料以及青藏高原东北侧地区同期17个站降水量观测资料,选取了初夏最干旱的3个年份(1962,199,1997年)和最湿润的3个年份(1967,1984,1985年),分析计算了初夏典型干湿年东亚范围内500hPa平均位势高度场,风矢场、涡度场和散度场,指出青藏高原东北侧初夏干旱和多雨与中高纬环流特征有关,表现在物理量场上有显差  相似文献   

10.
宁夏春季沙尘暴与北极海冰之间的遥相关关系   总被引:11,自引:3,他引:11  
根据宁夏沙尘暴发生次数资料、北极海冰密集度资料和NCEP/NCAR再分析500hPa、850hPa高度场、风场资料,得出了宁夏春季沙尘暴发生次数的变化规律及其与北极海冰面积之间的年代际和年际相关关系,发现宁夏春季沙尘暴发生次数与欧亚大陆北部的喀拉海、巴伦支海和格陵兰海冰面积之间存在较显著的年代际、年际相关关系。通过合成和相关分析知,宁夏春季沙尘暴偏多、偏少状况有明显不同的环流背景场,秋季格陵兰海冰异常变化通过影响其后一段时间的大气环流背景场,从而对宁夏沙尘暴产生影响。初步得出当格陵兰海秋季海冰面积增大(减小),次年春季蒙古至西伯利亚一带500hPa、850hPa高压场降低(升高),风场有明显的气旋性(反气旋性)特点,在宁夏至新疆一带西风明显偏强(偏弱),说明冷空气活动次数偏多(少),对应宁夏春季沙尘暴发生次数偏多(少)。通过海冰将全球气候变暖和宁夏(我国北方)沙尘暴总减少趋势联系起来,初次提出在环境总体恶化情况下,我国沙尘暴发生次数总体趋于减少,很可能是全球气候变暖所致。  相似文献   

11.
The spatial and temporal variations of daily maximum temperature(Tmax), daily minimum temperature(Tmin), daily maximum precipitation(Pmax) and daily maximum wind speed(WSmax) were examined in China using Mann-Kendall test and linear regression method. The results indicated that for China as a whole, Tmax, Tmin and Pmax had significant increasing trends at rates of 0.15℃ per decade, 0.45℃ per decade and 0.58 mm per decade,respectively, while WSmax had decreased significantly at 1.18 m·s~(-1) per decade during 1959—2014. In all regions of China, Tmin increased and WSmax decreased significantly. Spatially, Tmax increased significantly at most of the stations in South China(SC), northwestern North China(NC), northeastern Northeast China(NEC), eastern Northwest China(NWC) and eastern Southwest China(SWC), and the increasing trends were significant in NC, SC, NWC and SWC on the regional average. Tmin increased significantly at most of the stations in China, with notable increase in NEC, northern and southeastern NC and northwestern and eastern NWC. Pmax showed no significant trend at most of the stations in China, and on the regional average it decreased significantly in NC but increased in SC, NWC and the mid-lower Yangtze River valley(YR). WSmax decreased significantly at the vast majority of stations in China, with remarkable decrease in northern NC, northern and central YR, central and southern SC and in parts of central NEC and western NWC. With global climate change and rapidly economic development, China has become more vulnerable to climatic extremes and meteorological disasters, so more strategies of mitigation and/or adaptation of climatic extremes,such as environmentally-friendly and low-cost energy production systems and the enhancement of engineering defense measures are necessary for government and social publics.  相似文献   

12.
正While China’s Air Pollution Prevention and Control Action Plan on particulate matter since 2013 has reduced sulfate significantly, aerosol ammonium nitrate remains high in East China. As the high nitrate abundances are strongly linked with ammonia, reducing ammonia emissions is becoming increasingly important to improve the air quality of China. Although satellite data provide evidence of substantial increases in atmospheric ammonia concentrations over major agricultural regions, long-term surface observation of ammonia concentrations are sparse. In addition, there is still no consensus on  相似文献   

13.
Observed daily precipitation data from the National Meteorological Observatory in Hainan province and daily data from the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis-2 dataset from 1981 to 2014 are used to analyze the relationship between Hainan extreme heavy rainfall processes in autumn (referred to as EHRPs) and 10–30 d low-frequency circulation. Based on the key low-frequency signals and the NCEP Climate Forecast System Version 2 (CFSv2) model forecasting products, a dynamical-statistical method is established for the extended-range forecast of EHRPs. The results suggest that EHRPs have a close relationship with the 10–30 d low-frequency oscillation of 850 hPa zonal wind over Hainan Island and to its north, and that they basically occur during the trough phase of the low-frequency oscillation of zonal wind. The latitudinal propagation of the low-frequency wave train in the middle-high latitudes and the meridional propagation of the low-frequency wave train along the coast of East Asia contribute to the ‘north high (cold), south low (warm)’ pattern near Hainan Island, which results in the zonal wind over Hainan Island and to its north reaching its trough, consequently leading to EHRPs. Considering the link between low-frequency circulation and EHRPs, a low-frequency wave train index (LWTI) is defined and adopted to forecast EHRPs by using NCEP CFSv2 forecasting products. EHRPs are predicted to occur during peak phases of LWTI with value larger than 1 for three or more consecutive forecast days. Hindcast experiments for EHRPs in 2015–2016 indicate that EHRPs can be predicted 8–24 d in advance, with an average period of validity of 16.7 d.  相似文献   

14.
Based on the measurements obtained at 64 national meteorological stations in the Beijing–Tianjin–Hebei (BTH) region between 1970 and 2013, the potential evapotranspiration (ET0) in this region was estimated using the Penman–Monteith equation and its sensitivity to maximum temperature (Tmax), minimum temperature (Tmin), wind speed (Vw), net radiation (Rn) and water vapor pressure (Pwv) was analyzed, respectively. The results are shown as follows. (1) The climatic elements in the BTH region underwent significant changes in the study period. Vw and Rn decreased significantly, whereas Tmin, Tmax and Pwv increased considerably. (2) In the BTH region, ET0 also exhibited a significant decreasing trend, and the sensitivity of ET0 to the climatic elements exhibited seasonal characteristics. Of all the climatic elements, ET0 was most sensitive to Pwv in the fall and winter and Rn in the spring and summer. On the annual scale, ET0 was most sensitive to Pwv, followed by Rn, Vw, Tmax and Tmin. In addition, the sensitivity coefficient of ET0 with respect to Pwv had a negative value for all the areas, indicating that increases in Pwv can prevent ET0 from increasing. (3) The sensitivity of ET0 to Tmin and Tmax was significantly lower than its sensitivity to other climatic elements. However, increases in temperature can lead to changes in Pwv and Rn. The temperature should be considered the key intrinsic climatic element that has caused the "evaporation paradox" phenomenon in the BTH region.  相似文献   

15.
Storms that occur at the Bay of Bengal (BoB) are of a bimodal pattern, which is different from that of the other sea areas. By using the NCEP, SST and JTWC data, the causes of the bimodal pattern storm activity of the BoB are diagnosed and analyzed in this paper. The result shows that the seasonal variation of general atmosphere circulation in East Asia has a regulating and controlling impact on the BoB storm activity, and the “bimodal period” of the storm activity corresponds exactly to the seasonal conversion period of atmospheric circulation. The minor wind speed of shear spring and autumn contributed to the storm, which was a crucial factor for the generation and occurrence of the “bimodal pattern” storm activity in the BoB. The analysis on sea surface temperature (SST) shows that the SSTs of all the year around in the BoB area meet the conditions required for the generation of tropical cyclones (TCs). However, the SSTs in the central area of the bay are higher than that of the surrounding areas in spring and autumn, which facilitates the occurrence of a “two-peak” storm activity pattern. The genesis potential index (GPI) quantifies and reflects the environmental conditions for the generation of the BoB storms. For GPI, the intense low-level vortex disturbance in the troposphere and high-humidity atmosphere are the sufficient conditions for storms, while large maximum wind velocity of the ground vortex radius and small vertical wind shear are the necessary conditions of storms.  相似文献   

16.
正AIMS AND SCOPE Atmospheric and Oceanic Science Letters (AOSL) publishes short research letters on all disciplines of the atmosphere sciences and physical oceanography.  相似文献   

17.
《大气和海洋科学快报》2014,7(6):F0003-F0003
AIMS AND SCOPE
Atmospheric and Oceanic Science Letters (AOSL) publishes short research letters on all disciplines of the atmosphere sciences and physical oceanography. Contributions from all over the world are welcome.  相似文献   

18.
《大气和海洋科学快报》2014,(5):F0003-F0003
AIMS AND SCOPE Atmospheric and Oceanic Science Letters (AOSL) pub- lishes short research letters on all disciplines of the atmos- phere sciences and physical oceanography. Contributions from all over the world are welcome.  相似文献   

19.
20.
正Aims Scope Advances in Atmospheric Sciences(AAS)is an international journal on the dynamics,physics,and chemistry of the atmosphere and ocean with papers across the full range of the atmospheric sciences,co-published bimonthly by Science Press and Springer.The journal includes Articles,Note and Correspondence,and Letters.Contributions from all over the world are welcome.  相似文献   

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