monsoon zone 中文意思是什麼

monsoon zone 解釋
季風帶
  • monsoon : n. 1. 季（節）風〈在印度洋和亞洲南部5-9月自西南、10-12月自東北吹的風〉。2. （印度的）雨季,夏季季風期。
  • zone : n 1 【地理】（地）帶。2 區域，范圍，界。3 〈古、詩〉（腰）帶。4 圈，環帶。5 【數學】（球面）帶；...
  1. The paper concludes that the changing rate of ndvi of rain forest in tropic is the smallest, the changing curve is smooth, while the changing rate of ndvi of the deciduous broad leaf forest in warm - temperate zone is the largest the change of ndvi is the most conspicuous in winter and spring ( especially in april ) while is not conspicuous in summer and autumn by analyzing the change of ndvi along latitude using the ndvi value of different vegetation types along the same longitude. the vegetation index from warm temperate zone to semitropical zone has obvious transition, while other areas have no distinct change by analyzing the change of ndvi from temperate zone to semitropical zone to tropical zone using ndvi averagejn the same time it is concluded that the sink value in the beginning of the year 1995 is from the influence of the monsoon in east of china by analyzing the ndvi curve of several typical needle leaf forests. the relation between ndvi value and temperature is conspicuous while the relation of precipitation is less or not by analyzing the relation between ndvi and temperature and precipitation finally it can get the conclusion that the change of river area is the smallest, the change of sienna area is the greatest by analyzing two phases of tm data in 1987 and 1997 with rs technic

    利用從同一經度的不同森林類型ndvi值分析，沿緯度方向ndvi變化可得出， ndvi在冬春季變化最明顯（尤其是在4月份最大） ，而在夏季和秋季變化不明顯。利用ndvi均值進行分析，從暖溫帶到亞熱帶到熱帶的變化情況發現，從暖溫帶到亞熱帶ndvi指數形成明顯的階躍，而其它區域沒有太大的變化，同時對幾種典型的針葉林曲線分析可知其年初的凹值源自於我國東部季風的影響。利用ndvi數據分析其與月均溫度與降水的相關性得出與溫度相關性較為顯著，而與降水相關性不顯著或無相關性。
  2. Jinggangshan boasts a large area of mountains with rich vegetation. the streams enjoy a strong flow and a great drop ; therefore, within the scenic zone there are over 100 waterfalls, grand and marvelous. the landscape of the eighteen giant waterfalls of five large pools, attracts thousands of visitors from home and abroad. located in subtropical monsoon climate zone, jinggangshan is abundant in precipitation

    在兩級地形分界處，相咫尺之地往往相對高差達四五百米，地勢急轉直下，一落千丈，著名的五大哨口就屹立在地勢轉折地帶的險山要隘上，舊時進出井岡山中心- -茨坪的五條主要山道即在此險道之中。
  3. Suqian has the monsoon climate of warm temperate zone, with abundant sunshine and rainfall. its annual temperate averages 14 and the annual average precipitation is 913 mm

    宿遷屬暖溫帶季風性氣候，光照充足，雨水豐沛，年均氣溫14 ，年均降雨量913毫米。
  4. Concentrations of total suspended matter ( ctsm ) is unanimous with observational data and other scholars " researching results. the distribution of ctsm is higher along coast than other areas there is a tongue - like zone with high ctsm from north to southeast. the transport simulation result reveals that sm can spread to the okinawa trough for enough sea water mixing in winter. but in summer. sm can not traverse the big water barrier of kushino for different circulation character. this difference is probably related to the shifting n - s monsoon

    懸浮體輸送表明，在冬季，懸浮體除了在陸架上發生擴散外，由於海水的強烈混合作用和環流的季節性變化，部分中、底層懸浮體可擴散至沖繩海槽甚至西太平洋;在夏季，由於海水層化及夏季環流特徵，懸浮體基本不能穿越黑潮這一水障，這一差異可能是由於季風和不同環流特徵所引起的。
  5. Climate : this zone mostly belongs to the subtropical monsoon climate, where four seasons are distinguishable, mild climate, winter is not too cold, summer is not too hot, rain fall is abundant

    氣候：大多屬于中亞熱帶季風濕潤氣候，四季分明，氣候溫和，冬無嚴寒，夏無酷暑，雨量充沛。
  6. Climate : located in the temperate zone of east asia, binzhou has a sub - humid continental monsoon climate featuring four distinct seasons

    氣候特點：屬東亞暖溫帶亞濕潤大陸性季風氣候，冬冷夏熱，雨熱同期，四季分明。
  7. When the tcf in nwp is high, the bengal bay cef which located at 90 e is strong and the new guinea cef located at 150 e is weak ; there is a anti - cyclonic circulation near the equator. the equatorial buffer zone is fortified : it is propitious to the equatorial anticyclones activated and push monsoon trough to higher latitude, this circulation pattern can promote the genesis of tc in nwp

    多熱帶氣旋年，位於90 e附近的孟加拉灣越赤道氣流顯著增強，而位於150 e附近的新幾內亞越赤道氣流異常偏弱；在赤道附近存在一個異常的反氣旋性環流，赤道緩沖帶較強，有利於赤道高壓的活躍，季風槽被推向較高緯度，從而有利於熱帶氣旋的生成。
  8. Guilin is in subtropical and monsoon zone with warm and moist surrounding, so it is not very cold in winter and not very hot in summer

    桂林圍繞著亞熱帶和溫暖潮濕的季風地帶，因此在冬天氣溫不是很冷，夏天不是很熱。
  9. Qinling is the supreme mountains on the east of orient, and it lie on the border of monsoon zone, so qinling moutains play crucial role to the climate chang on the world

    秦嶺作為亞洲東部最高山地，又處于季風邊緣帶決定了它在我國乃至全球區域氣候、環境變化中有著舉足輕重的作用。
  10. Suqian has the monsoon climate of warm temperate zone. its annual temperature averages 14 and the annual average precipitation is 913mm

    宿遷屬暖溫帶季風性氣候，年均氣溫14 ，年均降雨量913毫米。
  11. Interdecadal fluctuations of the monsoon s boundary zone in the northern china

    中國北方季風邊緣區邊界位置的年代際變化
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