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英語人>網(wǎng)絡(luò)例句>monsoon 相關(guān)的網(wǎng)絡(luò)例句
monsoon相關(guān)的網(wǎng)絡(luò)例句

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與 monsoon 相關(guān)的網(wǎng)絡(luò)例句 [注:此內(nèi)容來源于網(wǎng)絡(luò)欧美性爱视频在线观看精品,僅供參考]

Anomalous anticyclone at the upper level is form in response to the enhanced convective heating off the equator, resulting in increased geopotential height and temperature over the Tibetan Plateau and in favor of the early BOB seasonal transition. Another effect of Positive SST anomalies over the Warm Pool is to induce anomalously strong zonal monsoon circulation. The anomalous zonal monsoon circulation strengths the southerlies in upper levels due to Coriolis force. Thus the enhanced warm meridional advection in connection with the warming over the Tibetan Plateau lead to early seasonal transition over the BOB region.

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The results show that the regional climate model can simulate East Asia summer monsoon system pretty well; the spatial distributions and the seasonal cycle of the surface air temperature and monsoon rain belt are in reasonable agreement with the observation.

并對區(qū)域氣候模式對東亞當代氣候模擬進行了分析射一射人人操一操,結(jié)果表明區(qū)域氣候模式能較好地模擬我國大陸地區(qū)顯著的季風氣候特點18禁片免费网站在线看,模擬的地面溫度和季風雨帶的空間分布和季節(jié)變化都與觀測較為一致,模擬結(jié)果反映了區(qū)域尺度下墊面強迫的影響美女视频在线观看永久免费,模擬出了遠比全球模式更為詳盡的區(qū)域氣候細節(jié)特征免费看国产黄A片在线。

E. , approximately four months; 2 the active periods occur much longer than the non-active periods; the main climatic characteristics of the non-active periods, compared with the active periods, is weaker monsoon with westerlies at 850-hPa and easterlies at 200-hPa on the deviation fields of circulations over the SCS (active time minus non-active time); it is warmer in the active periods than in the non-active periods at lower and upper levels; 3 in most circumstances, the low frequency vibrations of the summer monsoon and its rainfall are quite in phase.

2其中活躍期出現(xiàn)時間要比非活躍期長的多。與活躍期相比非活躍期主要氣候特征表現(xiàn)為季風的減弱欧美一级aa黄片系列精品99,在環(huán)流的偏差場上在南海上空850hPa上為西風在线国产黄色站,200hPa上為東風,活躍期高低空都比非活躍期要暖一些色综合色狠狠天天综合大色。(3)在多數(shù)情況下夏季風和夏季風降水的30-60天的低頻振蕩比較一致东北粗口熟女丰满高潮。

Luozha River is a first branch of Lancang River in its middle section. A less known deciduous monsoon forest was recently discovered on the dry-hot banks of Luozha River. The deciduous monsoon forest is 15-20 m tall with Lannea coromandelica Colona floribunda. Mallotus philippensis as the dominant tree species, and Microstegium ciliatum Eupatorium odoratum、Ageratum conyzoides are the dominant species in the shrub-herb layer.

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German climate scientists Haug, led by Germany, China, the United States study group to carry out core Leizhou Peninsula paleoclimate research, so as to equip the ancient East Asian winter monsoon intensity, one of which concluded that: Datang and the Arab fighting in the Asian city of Talas, Tang Jun, defeated the Tang Empire began to decline, just at the time of the dry monsoon abnormal dry spells.

德國氣候科學家豪格率領(lǐng)的德、中456亚洲视频在线观看、美研究小組免费www你懂的网站视频,以雷州半島的巖芯進行古氣候研究中国野外一级视频片,從而掌握東亞古代冬季季風強度,其中一個結(jié)論是:大唐與阿拉伯激戰(zhàn)于中亞重鎮(zhèn)怛邏斯自拍欧美日韩制服视频,唐軍大敗国产一级黄色视频免费看,唐帝國開始衰落,其時恰好處于季風異常的少雨干旱期一级一片免费观看。

For the climatic characteristics of the maintenance of the SCS summer monsoon, results show: 1 according to the 40-year means, the maintenance period of the SCS summer monsoon is around 25 pentads, i.

對于南海夏季風維持期的氣候特征,研究發(fā)現(xiàn):(1)就四十年平均而言熟女强奸乱伦电影,南海夏季風維持時間大約為二十五候約四個月欧美十日韩十国产。

We define the active periods of the SCS summer monsoon as the time when the the onset condition of the SCS summer monsoon is satisfied in successive pentads, else the non-active periods when the onset condition is at fault.

我們將連續(xù)滿足南海夏季風建立條件的侯稱為活躍期,而將連續(xù)不滿足南海夏季風建立條件的侯稱為非活躍期1级黄色免费片。

Asian summer monsoon, one of the earth′s most energetic weather events, undoubtedly plays a key role in the variability of the general circulation. In this paper, through both calculation for the correlation coefficients between the monsoon indices and the geopotential height and the anomalous composite of the strong or weak ASM pentads, it is shown that the activity of the ASM...

本文通過夏季風指數(shù)與北半球環(huán)流的相關(guān)計算以及強99这里只有精品首页、弱季風候北半球環(huán)流異常合成的分析發(fā)現(xiàn),亞洲夏季風的活動會激發(fā)北半球夏季大氣環(huán)流遙相關(guān)型性直播在线看黄网站,其主要相關(guān)中心均出現(xiàn)在季風區(qū)的下游地區(qū)青草视频在线播放精品无码,即從亞洲經(jīng)太平洋至北美洲一帶,除了表現(xiàn)出正負中心交替出現(xiàn)的波列狀結(jié)構(gòu)外在线观看国产,該遙相關(guān)型在太平洋地區(qū)還表現(xiàn)為一對南北向的偶極子異常型91人妻教师超碰,我們將這一遙相關(guān)型稱為亞洲太平洋北美型

During the four years study on the project, we develop a dynamical forecast model that describing the subtropical ridge surface. A new theory on the role of the land-sea thermal difference on the formation of the Subtropical High is advanced. It is concluded that in the summer subtropics over each continent and its adjacent ocean LO, SE, CO, and a double-dominant heating from west to east compose a LOSECOD heating quadruplet. The influence of the Eurasia continent on SH varies according to the seasonal variation. From the ideal numerical simulation it is shown the important role of the Eaiuan continent and the huge topography on the mechanism of formation and mantanence of the SH during the summer. It is verified by the numerical simulation that the extension of the subtropical continent into the tropics greatly enhances the " East Asian monsoon". Through the Rossby energy dissipation theory it is verified that the deep latent convective heating induces the onset of the South China Sea monsoon over the Bay of Bengal. The relationship and mechanism between the precipitaiton over the East Asia and the Subtropicla high is illustrated by the data. It is also found the close phase lock between the east-west shift of the SH and the disturbence of the east wind belt over the tropical troposphere. The interaction between the structure and activity feature of the SH and the Meiyu over the Yangtze-Huaihe river valley is revealed from the data. The numerical simulation verified the impact of the different SH pattern on the path of the typhoon.

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