克拉玛依夏季日最高气温与08时 850hPa温度的关系   总被引：2，自引：0，他引：2  

冀新琪 《沙漠与绿洲气象(新疆气象)》2005,28(4):12-13

根据克拉玛依40年气温观测资料,分析克拉玛依夏季日最高气温与08时850hPa温度的关系,寻找预报夏季日最高气温关键因子.  相似文献   

我国松花江流域和辽河流域降水的长期变化规律和未来趋势分析   总被引：5，自引：0，他引：5       下载免费PDF全文

李想李维京  赵振国 《应用气象学报》2005,16(5):593-599

利用1881～2002年我国东北地区的月、季降水资料,采用历史曲线分析、功率谱分析、小波变换等方法,重点分析了松花江流域和辽河流域降水的长期变化规律。结果表明:松花江流域和辽河流域的降水都存在着明显的年代际变化,松花江流域降水以27～30年周期为主,辽河流域降水周期比松花江流域略长,大概为35～38年左右。根据降水自身演变规律及自回归方法预测的结果,估计未来5～10年,松花江流域仍将处于少雨期,辽河流域少雨期维持时间可能会稍长一些。  相似文献   

非地转强迫对Fitow(0114)暴雨的影响   总被引：3，自引：3，他引：3  

李江南  闫敬华  魏晓琳  吴池胜  侯尔滨  王安宇 《气象学报》2005,63(1):69-76

利用非静力中尺度模式MM5对 0 114号台风Fitow从 2 0 0 1年 8月 31日 0 0时～ 9月 2日 0 0时 (UTC ,下同 )的降水过程进行了模拟研究。结果表明 ,MM5对Fitow登陆过程中暴雨落区和强度的模拟与实况比较一致。模拟结果较好地再现了暴雨的中尺度特征。正是维持少动的台风倒槽和嵌入其中的中小尺度系统相互作用造成了暴雨的发生、发展 ,而高、低空中尺度散度场的配置对暴雨有很好的指示意义。在华南台风暴雨区无论是高层还是低层 ,都存在很强的非地转作用 ,非地转涡度项对散度倾向项是重要的强迫因素 ;但非地转作用的实现与中高纬度地区有本质的区别 ,在低层非地转作用是由于强的位势场气旋涡度 (- 2  <0 )与弱的流场气旋涡度 (fζ >0 )不平衡产生的 ;而高层非地转作用是由于强的位势场反气旋涡度 (- 2  >0 )与弱的流场反气旋涡度 (fζ <0 )不平衡产生的。非地转作用是暴雨中尺度系统上升运动发展的触发机制。从动力学角度解释了用非地转 Q矢量散度场来判断暴雨落区要比用准地转 Q矢量散度场好的原因。  相似文献   

祁连山林区大气降水特征与森林对降水的截留作用   总被引：30，自引：3，他引：30  

常学向  赵爱芬  王金叶  常宗强  金博文 《高原气象》2002,21(3):274-280

通过对连山寺大隆林区定位站1975－2000年的降水特征与森林对降水的再分配分析，建立了祁连山大隆林区降水与温度，降水与湿度，林冠截留的关系式。该区多年平均降水量为433.5mm，年变幅在326.4-539.7mm;降水量最大出现在夏季，占全年降水量的65．70％；海拔高度每升高100m，年了量平均递增4．55％，林区温度和湿度均与降水有较好的拟合关系。青海云杉林与祁连圆柏林林冠对大气降水的平均截留率分别为37．5％，31．7％，灌木林的截留率平均高达66．5％。青海云杉林林冠层平均截留率随着降雨量的增大逐渐减小，当降雨量为18.67mm时，林冠截留量达到最大，为14.72mm；青海云杉树干径流量占降水量的0．51％，当降雨量超过12.0mm时，才开始产生树干径流。青海云杉林枯枝落叶层对降雨的截留量随降雨量级增加而增大，截留率则随降雨量减小而增大，枯枝落叶层所具有的截留降雨和调蓄降雨作用使祁连山林区基本不发生地表径流。分析结果表明，祁连山林区对水源涵养和水流出山的时间调控有重要意义。  相似文献   

黑龙江气候变暖的时空变化特征   总被引：15，自引：0，他引：15  

潘华盛  张桂华 《黑龙江气象》2002,(3):3-6,11

进入80年代以来，黑龙江气温明显变暖，近120年来年平均气温上升1.4℃，春季次之，气温突变在1990年前后，从年、各季平均气温变化趋势与全国北半球及全球气温变化进行比较，年及冬季我国增暖中心在黑龙江，春季增暖中心在内蒙古北部及黑龙江省；夏秋增暖不明显，但仍有上升趋势，近50年来，50～70年代黑龙江省及全国各大区域普遍增暖不明显，80年代开始黑龙江省增暖明显，三北地区次之，90年代黑龙江增暖更加明显，而全国及其他区域上升已达到80年代北方增温幅度，这里从黑龙江变暖的事实，突变时间，与全球、北半球、全国区域的气温及雪盖海温变化关系来揭示黑龙江气候变化的时空特点。  相似文献   

CLIMATOLOGICAL CHARACTERISTICS FOR THE ONSET OF ASIAN SUMMER MONSOON AS REVEALED BY HIRS-Tb12 AND DROUGHT AND FLOODS IN EASTERN CHINA     

施宁  蒋尚城  严明良 《热带气象学报(英文版)》2002,8(2):141-149

As shown in comparison and study of the HIRS-Tb12 data and conventional data, temperature, humidity and vertical motion are structured differently in the Southern and Northern Hemispheres, which are well depicted with the HIRS-Tb12 data. When high pressures rapidly decrease over the regions of South China Sea and Arabian Sea with the HIRS-Tb12 less than 200 W/m2, monsoons will set off in the South China Sea, Arabian Sea and Bay of Bengal, respectively. From a year of significant drought to one of significant floods, the trend of evolution is significantly different in the downdraft areas of the subtropical highs between the two hemispheres.  相似文献   

Atmospheric Surface-Layer Processes During the Total Solar Eclipse Of 11 August 1999     

Prakash M. Ramchandran  Radhika Ramchandran  K. Sen Gupta  S. M. Patil  P. N. Jadhav 《Boundary-Layer Meteorology》2002,104(3):445-461

The central path of the total solar eclipse (TSE) of 11 August 1999 mostly passedthrough a region of active monsoon in India, with the eclipse ending around localsunset. Measurements in the surface layer (SL) were carried out close to the eclipseaxis at Akola (20°42' N, 77°2' E) in central India. The globalradiation flux reaching the surface vanishes around totality at 1803:24 (LT), followedby a small recovery before again dipping to zero at sunset. The temperatures in the SL, and subsoil at 50-mm depth, show a local minimum with a lag of about 10 min after the second contact, whereas the lag appears to vanish when the temperature series is detrended. The SL exhibits near-neutral, though generally stable, conditions from about 1500 hr itself due to heavy cloud cover followed by the eclipse-induced cooling of the surface. The wind component across the eclipse axis vanishes at totality, the wind vector aligning with the azimuth of the traversing moon shadow. The deceleration of the mean flow can be due to the combined effect of the colder surface and downward heat flux, where the locally altered horizontal temperature gradients may cause, as in this instance, the cessation of the cross flow.The oscillations in temperature and wind that show significant peaks, around 90–100 min as well as the semi-period of the eclipse near 60 min, persist for several hours past the eclipse event. A fresh analysis of the published data on the TSE of 7 March 1970 shows spectral peaks in the temperature nearly coincident with those already reported from the surface pressure records. The oscillations in the SL fields during the two TSE events are very similar implying that the source mechanism is also likely to be the same in both the cases.  相似文献   

Evolution of the fogwater composition in Strasbourg (France) from 1990 to 1999     

Pierre Herckes  Henri Wortham  Philippe Mirabel  Maurice Millet   《Atmospheric Research》2002,64(1-4)

The chemical composition of fogwater has been studied in the city of Strasbourg (France) from 1990 to 1999. During these years, fogwater samples have been collected and analysed for major ions and trace metals. This paper reports on the analysis of the collected dataset. The analysis revealed a significant decrease in acidity of approximately one pH unit over the course of the study. This decrease in acidity appears to be linked to a decrease in SO_2(g) and the resulting SO₄²⁻. Trace metal concentrations have also strongly decreased over the 10-year period. Pb concentrations, following the elimination of leaded gasoline, decreased by more than one order of magnitude.  相似文献   

江西银山多金属矿床伊利石的形成与流体成矿作用的初步研究   总被引：4，自引：0，他引：4  

李晓峰  华仁民  季俊峰  陆建军  刘盛祥  刘连文 《地质科学》2002,37(1):86-95

江西银山多金属矿床的热液蚀变粘土矿物主要由伊利石组成,伊利石主要由流体作用过程中长石的伊利石化形成,其结晶度与成矿流体作用密切相关.银山第1期铅锌银成矿作用,水/岩比相对较低,成矿流体以孔隙渗透为主,溶质迁移慢,形成含有少量膨胀层的伊利石;第2期铜金成矿作用,水/岩比相对较高,流体的运移方式以通道式或裂隙式为主,溶质迁移的速度快,形成不含膨胀层的伊利石.研究表明成矿作用过程中的伊利石化主要与铅锌银矿化有关,而绿泥石化与铜金矿化有关.  相似文献   

Study on effects of damping in laminated rubber bearings on seismic responses for a ⅛ scale isolated test structure     

Bong Yoo  Yang‐Hann Kim 《地震工程与结构动力学》2002,31(10):1777-1792

The effects of damping in various laminated rubber bearings (LRB) on the seismic response of a ?‐scale isolated test structure are investigated by shaking table tests and seismic response analyses. A series of shaking table tests of the structure were performed for a fixed base design and for a base isolation design. Two different types of LRB were used: natural rubber bearings (NRB) and lead rubber bearings (LLRB). Three different designs for the LLRB were tested; each design had a different diameter of lead plug, and thus, different damping values. Artificial time histories of peak ground acceleration 0.4g were used in both the tests and the analyses. In both shaking table tests and analyses, as expected, the acceleration responses of the seismically isolated test structure were considerably reduced. However, the shear displacement at the isolators was increased. To reduce the shear displacement in the isolators, the diameter of the lead plug in the LLRB had to be enlarged to increase isolator damping by more than 24%. This caused the isolator stiffness to increase, and resulted in amplifying the floor acceleration response spectra of the isolated test structure in the higher frequency ranges with a monotonic reduction of isolator shear displacement. Copyright © 2002 John Wiley & Sons, Ltd.  相似文献