机构地区:[1]Department of Atmospheric Sciences, Sun Yat-sen University, Guangzhou 510275, China [2]NanAo Observatory of Shantou Meteorological Bureau, Shantou 515900, China
出 处:《Chinese Science Bulletin》2010年第33期3818-3824,共7页
基 金:supported by the National Natural Science Foundation of China(40875020);the NSFC-Guangdong Joint Fund Program(U0733002);the National Basic Research Program of China(2009CB421404)
摘 要:Climatological relationships among the tropical cyclone(TC)frequency,duration,intensity and activity regions over the Western Pacific are explored based on long-term best track data.Frequent TC occurrence does not necessarily imply a long duration of TCs in the same periods.Three types of relationship between TC number and duration in the period 1945-2007 were identified in this study:low frequency and short duration during 1945-1955(Period I);high frequency and short duration in the 1960s(Period II);and high frequency and long duration in the 1990s(Period III).TC activity regions differed among the three periods.During Period I,the main activity regions were over the ocean east of the Philippines(120°-140°E).During period II,two prevailing storm tracks extended west-northwest between 110° and 147°E.During period III,TCs had an extensive activity region from 110° to 160°E.TC intensity is related closely to activity regions.Most strong TCs developed over the ocean far from the Philippines,and had a northwestward track.Our results also show that the relationships between TC frequency,duration and their active regions are modulated strongly by broad-scale vertical motion,geopotential height and horizontal wind anomalies.Climatological relationships among the tropical cyclone (TC) frequency, duration, intensity and activity regions over the Western Pacific are explored based on long-term best track data. Frequent TC occurrence does not necessarily imply a long duration of TCs in the same periods. Three types of relationship between TC number and duration in the period 1945-2007 were identified in this study: low frequency and short duration during 1945-1955 (Period I); high frequency and short duration in the 1960s (Period lI); and high frequency and long duration in the 1990s (Period I1/). TC activity regions differed among the three periods. During Period I, the main activity regions were over the ocean east of the Philippines (120^-140~E). During period II, two prevailing storm tracks extended west-northwest between 110~ and 147~E. During period III, TCs had an extensive activity region from 110~ to 160~E. TC intensity is related closely to activity regions. Most strong TCs developed over the ocean far from the Philippines, and had a northwestward track. Our results also show that the relationships between TC frequency, duration and their active re- gions are modulated strongly by broad-scale vertical motion, geopotential height and horizontal wind anomalies.
关 键 词:西太平洋地区 持续时间 活动区域 热带气旋 气候关系 低频率 强度 跟踪数据
分 类 号:P444[天文地球—大气科学及气象学] TU238.2[建筑科学—建筑设计及理论]
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