dry monsoon 中文意思是什麼
dry monsoon
解釋
冬季風-
Setenaly according to the analyses from selected profiles, we know that, it is cold and dry in this region during the early holocene when east asian winter monsoon ' s influence is obvious, so, it is a transition period from sand deposit to sandy soil deposit, when the layers become thinner gradually from north to south. during middle holocene, it is warm and humid, influenced evidently by east asian summer monsoon, so, it is an obivious pedogenesis, when there are generally well - developped holecene palaeosol ( so ) from north to south, and the pedogenesis in the south is better than that in the north, the soil is also thicker than that of the north. from late holocene to now, the climate changes to be dry and cold, but its changing scope is smaller than that of last glacial period
2 、就所選剖面分析來看，本區在全新世早期氣候回返，相對較寒冷乾燥，東亞冬季風影響較明顯，此時為沙層堆積向砂質土壤過渡，自北至南堆積的沙粒漸細；全新世中期氣候溫暖濕潤，東亞夏季風影響顯著，此時為明顯的成壤期，表現在自北至南普遍可見發育較好的黑壚土層，且南部的成壤作用比北部好，土壤的厚度也要大；全新世晚期至今，氣候向乾冷方向轉化，但變化幅度遠小於末次冰期。 -
Winter brings cool, dry weather with many bright days, while during the summer - the monsoon season, the weather is warm and humid, and rainstorms can be expected. between july and september is the most likely time for typhoons. there are five levels of tropical cyclone warning starting with 1 ( the lowest and least intense ) through 3, 8, 9 to 10 ( the highest and most critical )
香港的冬季大部份是乾爽涼快的晴天；夏季則屬季侯風季節，天氣溫暖潮濕，時有暴風雨， 7月至9月期間為香港的臺風季節，熱帶氣旋分為5級，由1級（最低程度及風力最弱）開始，然後可遞升至3 、 8 、 9及10級（最高程度及風力最強） 。 -
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 the eastern monsoon region, transition of summer rainfall from below normal to above normal in the lower yangtze river in 1979 was accompanied with dry trends in north china and south china
與全球增暖相聯系的是：我國微量降水在空間上表現為一致的減少趨勢，我國北方寒潮事件顯著減少，冷夜和冷日的減少與暖夜和暖日的增多並存，以及極端強降水有增多的趨勢。 -
The study on precipitation field pointed out that most precipitation occurs in the monsoon area where exists the obvious rainy and dry season
指出降水量最大的區域主要在季風區，在季風降水區域，有明顯的雨季和旱季。
分享友人