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261.
贵州与印度的夏季风的异同分析 总被引:3,自引:0,他引:3
季风作了气象科学的一个重要课题,许多人都作了大量研究,中国和印度均处于季风区,印度季风和中国季风的研究已作了大量研究,揭露了不少事实,但中国季风的研究多指我国的东部,而贵州位于我国西南部,地处东亚季风和印度季风之间的过渡区,因此,对贵州省的论及较少,从气候的角度出发,把贵州和印度的季风的某些特征量,如降雨、风、环流等进行对比分析,在一定程度上反映了贵州和印度夏季风的主要异同。 相似文献
262.
Motoyoshi Ikeda 《极地研究(英文版)》2008,19(2):212-217
The sea ice cover in the Arctic Ocean has been reducing and hit the low record in the summer of 2007. The anomaly was extremely large in the Pacific sector. The sea level height in the Bering Sea vs. the Greenland Sea has been analyzed and compared with the current meter data through the Bering Strait. A recent peak existed as a consequence of atmospheric circulation and is considered to contribute to inflow of the Pacific Water into the Arctic Basin. The timing of the Pacific Water inflow matched with the sea ice reduction in the Pacific sector and suggests a significant increase in heat flux. This component should be included in the model prediction for answering the question when the Arctic sea ice becomes a seasonal ice cover. 相似文献
263.
This study presents a new way to identify the sensitive areas for typhoon adaptive observations, that is, sensitive areas are determined by invoking the negative anomalies of moist potential vorticity (MPV). It is found that the areas of negative MPV are the symmetric instability areas and can be taken as sensitive areas for typhoon adaptive observations. Three typhoons in 2008, Nuri, Fung-wong, and Fengshen, were simulated with the help of MM5 model. It is shown that these typhoons are well simulated in the first 12 hours. Based on these investigations, the calculations of MPV are carried out sequentially. The result shows that the negative maxima of MPV are always around the typhoon eyes for all the cases, which means that the sensitive areas are also near them all the time. 相似文献
264.
265.
266.
华南前汛期降水异常及其环流特征分析 总被引:9,自引:2,他引:7
利用国家气候中心整编的中国160站的月平均降水资料和美国NCEP/NCAR的再分析资料,分析华南前汛期降水的异常及其环流特征。文中取“九五”重中之重项目执行组指出的华南地区的16站来代表华南地区,侧重分析了华南前汛期降水异常的年际、年代际变化特征及华南前汛期多、少雨年同期的环流特征。研究发现:华南地区降水的季节分布呈现双峰型,两个峰值分别在6月和8月。华南前汛期近50年的总的降水趋势变化不明显。1950年代前期和1960年代中期—1980年代中为相对多雨期,而1950年代中期—1960年代中期以及1980年代中期—1990年代初为相对少雨期,1990年代为正常波动期。华南前汛期降水存在3 a、5 a、7 a、14 a的周期。在分析华南前汛期多、少雨年大气环流场的特征时发现:华南前汛期多雨年时南亚高压和副高都偏弱,华南地区低层的水汽通量辐合加强,而且低空辐合,高空辐散,气流上升运动加强,容易形成降水;而少雨年的情况恰恰相反。 相似文献
267.
A nested-model system is constructed by embedding the regional climate model RegCM3 into ageneral circulation model for monthly-scale regional climate forecast over East China. The systematicerrors are formulated for the region on the basis of 10-yr (1991-2000) results of the nested-model system,and of the datasets of the Climate Prediction Center (CPC) Merged Analysis of Precipitation (CMAP) andthe temperature analysis of the National Meteorological Center (NMC), U.S.A., which are then used forcorrecting the original forecast by the system for the period 2001-2005. After the assessment of the originaland corrected forecasts for monthly precipitation and surface air temperature, it is found that the correctedforecast is apparently better than the original, suggesting that the approach can be applied for improvingmonthly-scale regional climate dynamical forecast. 相似文献
268.
269.
Tidal effects on temperature front in the Yellow Sea 总被引:5,自引:0,他引:5
Temperature front (TF) is one of the important features in the Yellow Sea, which forms in spring, thrives in summer, and fades
in autumn as thermocline declines. TF intensity ⋎S
T
⋎ is defined to describe the distribution of TF. Based on the MASNUM wave-tide-circulation coupled model, temperature distribution
in the Yellow Sea was simulated with and without tidal effects. Along 36°N, distribution of TF from the simulated results
are compared with the observations, and a quantitative analysis is introduced to evaluate the tidal effects on the forming
and maintaining processes of the TF. Tidal mixing and the circulation structure adapting to it are the main causes of the
TF.
Supported by the National Basic Research Program of China (No. G1999043809) and the National Science Foundation of China (No.
49736190). 相似文献
270.
D.X.HU 《中国海洋湖沼学报》2004,22(3):J001-J002
Ocean circulation in the Yellow and East China Seas is very rich in mesoscale phenomena, such as eddies, fronts, upwellings, river plumes, etc. Among others, having drawn tremendous attention from oceanographic community in the past for nearly 50 years are mainly the Yellow Sea Cold Water Mass (YSCWM) and its related circulation, the Yellow Sea Warm Current (YSWC), the East China Sea 相似文献