WNP

基本解釋

Our results indicate that the rotational wind component is the key factor affecting Typhoon activity in the WNP.
研究結果顯示，旋轉風分量是影響西北太平洋臺風活躍度之關鍵。
Abstract: The characteristics of tropical cyclone (TC) over the western North Pac ific (WNP) in 2008 were reviewed, and its causation was analyzed.
中文摘要: 對2008年西北太平洋及我國南海熱帶氣旋的活動特征進行總結，并從多方面分析其成因。
To assess dynamic impacts of monsoonal circulation on TCs formation in different areas over the WNP, the WNP is divided into four domains.
2.;本研究還把WNP劃分4個不同的區(qū)域;以此深入研究熱帶西太平洋不同區(qū)域中TC生成的動力作用。
The WNP anticyclone forms in the El Nino growing autumn, grows in the El Nino mature winter and the following spring, and decays in the subsequent summer, respectively.
WNP反氣旋形成于El Nino發(fā)展期的秋季,發(fā)展于成熟期的冬季和次年春季,衰減于次年夏季。
A comparison with previous results indicates that a similar spatial and temporal distribution of SST anomalies is also associated with the onsets of both the WNP and South China Sea (SCS) monsoons.
與以前的研究結果進行了比較，說明上述海溫異常的時空分布也與熱帶西太平洋和南海季風的爆發(fā)早晚相關聯(lián)。