indian monsoon 中文意思是什麼
indian monsoon
解釋
印度季風-
( 4 ) summer rainfall anomalies in north china relates to the indian summer monsoon, the south sea monsoon, sub - tropical anticyclone, south asian anticyclone and cold air anomaly
（ 4 ）華北地區夏季降水異常與印度西南季風、南海東南季風、副熱帶高壓、南亞高壓及冷空氣異常都密切相關。 -
( 5 ) there exists close relationship between the meiyu period precipitation in jianghuai valleys and the anomalies of subtropical summer monsoon, the anomalies of cold air, not the same so the indian summer monsoon
（ 5 ）江淮地區梅雨期降水與東亞副熱帶季風、北方冷空氣異常密切相關，與印度西南季風關系並不密切。 -
The summer rainfall anomaly of north china is closely related to indian low, west pacific subtropical high, westerly troughs and ridges in mid - latitude, south asia high, subtropical monsoon circulation and cold air activity on the corresponding period, and similar circulation pattern also appears in the preceding spring
結果表明： （ 1 ）華北夏季降水異常與同期印度低壓、西太平洋副高、中緯度西風槽脊、南亞高壓、副熱帶季風環流和冷空氣活動的異常都密切相關。華北夏季降水異常年春季的環流特徵與夏季類似。 -
Kunming belongs to the low latitude plateau mountainous country monsoon climate, because of locating in the western region of yungui plateau, the degree of latitude is low, the elevation is high, there are the wumeng mountains to be as the natural screen in the north, separating the cold air to go down south, the whole area is subjected to influence that come from southwest and warm moisture of indian ocean s flow more, adding there are the plateau lakes to regulate degree of humidity, becoming the four seasons of " summer have no intense heat, winter have no strict and cold ", such as pleasant weather of the spring
昆明屬低緯高原山地季風氣候，由於地處雲貴高原西部，緯度低，海拔高，北部有烏蒙山等群山作為天然屏障，阻隔南下的冷空氣，全區多受來自印度洋西南暖濕氣流的影響，加之有高原湖泊滇池陽宗海調節溫濕度，形成「夏無酷暑，冬無嚴寒」四季如春的宜人氣候。年平均氣溫為14 . 5 ，最熱月平均氣溫19 . 7 ，最冷月平均氣溫7 . 5 ，年平均日照時數為2400多小時。 -
( 3 ) when the heat source over the bay of bengal is abnormally strong ( weak ), the sourthern asian high extends westward ( eastward ), and the western pacific subtropical high extends eastward ( westward ), and the indian summer monsoon is stronger ( weaker ), and the eastern asian tropical summer monsoon is weaker ( stronger )
（ 3 ）當孟加拉灣熱源異常強（弱）時，南亞高壓偏西（東） ，西太平洋副熱帶高壓位置偏東（西） ；印度夏季風偏強（弱） ，東亞熱帶季風偏弱（強） 。 -
When the heat source over the bay of bengal was abnormally strong ( weak ), the southern asian high extended westward ( eastward ), and the western pacific subtropical high extended eastward ( westward ), and the indian summer monsoon was stronger ( weaker ), and the eastern asian tropical summer monsoon was weaker ( stronger )
當孟加拉灣熱源異常強（弱）時，南亞高壓偏西（東） ，西太平洋副熱帶高壓位置偏東（西） ；印度夏季風偏強（弱） ，東亞熱帶季風偏弱（強） 。 -
When the heat source over philippines is abnormally weak, the southern asian high becomes only one part and its location extends southward, the indian summer monsoon is stronger, the eastern asian tropical summer monsoon is weaker, and the western pacific subtropical high extends southward ; the influence of the heat source strong anomalies over philippines on the east part of the southern asian high and the western pacific subtropical high and the east asian tropical summer monsoon is significant and whic h on the indian summer monsoon is not significant ; the influence of the heat source weak anomalies over philippines on the east asian tropical summer monsoon and the indian summer monsoon and the western pacific subtropical high and the southern asian high is significant
東亞熱帶季風加強，南亞季風也有所加強，西太平洋副熱帶高壓位置偏北；當夏季菲律賓熱源異常減弱時，南亞高壓只表現為一個部分，且位置偏南，南亞季風加強，東亞熱帶季風減弱，西太平洋副熱帶高壓位置偏南。夏季菲律賓熱源異常強年，東部的南亞高壓異常顯著，副熱帶高壓位置異常偏北也達到顯著水平，東亞熱帶季風的加強是顯著的，而南亞季風的加強並不顯著；而熱源異常減弱時，東亞熱帶季風的減弱、南亞季風的加強都達到顯著水平，副熱帶高壓、南亞高壓的位置異常偏南也是顯著的。 -
In dry ( wet ) year, mongolia high was stronger ( weaker ), indian low was later ( sooner ) and weaker ( stronger ), baikal blocking high was stronger ( weaker ), asian summer monsoon was weaker ( stronger ), west pacific subtropical high leaned toward north ( south ), east ( west )
這些異常表現為：旱（澇）年蒙古高壓異常偏強（弱） ，印度熱低壓建立晚（早）且較弱（強） ，貝加爾湖阻塞高壓較強（弱） ，亞洲夏季風偏弱（強） ，西太平洋副熱帶高壓偏南（北） ，偏東（西） 。 -
In winter ( january ), there are four nearly latitudinal moisture transport belts ( channel ) over asian - australian monsoon region. they are closely related with the easterlies and westerlies over southern hemisphere and northern hemisphere. in boreal winter, asian monsoon region is moisture source ; the cross equatorial moisture transport channels transport the moisture to australian monsoon and south indian ocean from asian monsoon region
主要結論如下： （ 1 ）冬季（ 1月）的水汽輸送形勢與南北半球東、西風帶緊密聯系，主要有四條近似緯向分佈的垂直積分的強水汽輸送帶，越赤道輸送將水汽從亞洲季風區輸送到南半球澳大利亞季風區和南印度洋季風區，亞洲季風區為水汽源區。 -
The government of the western indian state of maharashtra yesterday banned the manufacture, sale and use of all plastic bags, saying they choked drainage systems during last month ' s monsoon rains
位於印度西部的馬哈拉施特拉省地方政府在24日宣布將禁止製造、販售和使用所有的塑膠袋，因為它們在上個月的雨季里嚴重堵塞排水系統。 -
During 1950 ~ 1976 / 1977, the walker circulation over the tropical pacific and the vertical zonal monsoon circulation over the tropical indian ocean coupled at the oceanic continent, the same period when el nino occurs, the anomaly of the west wind over the tropical pacific can correlate with the departure of east wind over the tropical indian ocean through the two coupled vertical zonal circulation. but after 1976 / 1977, the updraft of the walker circulation moved eastward. locating at the north of australia. therefore the two vertical zonal circulation could n ' t coupled, and the anomaly of west wind and the departure of east wind could n ' t geared. in the result. the signal of enso decreased in indian ocean after 1976 / 1977
1951 1976 1977年，熱帶太平洋的walker環流和熱帶印度洋的緯向季風環流在海洋性大陸附近耦合，當elnino事件發生時，太平洋的西風異常可以通過這兩個緯向的垂直環流與印度洋的東風異常聯系起來，而1976 1977年以後，由於西太平洋walker環流上升支東移到澳大利亞北部，熱帶兩洋的緯向垂直環流無法耦合，熱帶太平洋elnino事件中的西風異常與熱帶印度洋的東風異常聯系減弱，所以1976 1977年以後， enso在熱帶印度洋的信號減弱了。 -
Monsoon rains and poor drainage enable the disease to thrive in many indian cities
季風降雨以及排水不暢，使得這種疾病仍在印度的許多城市中肆虐。 -
The tropical indian ocean, especially for the region north of 7, is strongly influenced by asia monsoon. in response to the seasonal reversal of wind, ocean currents also show obvious seasonal reversal with somali current most prominent
熱帶印度洋，尤其是7 s以北的印度洋，受亞洲季風的顯著影響，與季風對應，海洋環流也有很明顯的季節變化，最明顯的是索馬里海流的季節轉向。
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