气候与环境研究
氣候與環境研究
기후여배경연구
CLIMATIC AND ENVIRONMENTAL RESEARCH
2000年
4期
434-446
,共13页
南海夏季风%海-气交换%湍流通量
南海夏季風%海-氣交換%湍流通量
남해하계풍%해-기교환%단류통량
summer monsoon%air-sea exchange%turbulent flux
根据1998年“南海季风试验(SCSMEX)”强化观测期间“实验3号”和“科学1号”科学考察船船基大气海洋自动观测系统两点连续观测的大气、海洋资料,使用考虑到风速和大气层结影响的整体输送公式计算海-气间的湍流通量交换。根据计算结果分析南海夏季风期间海表大气要素和海温日均值的逐日变化、海洋向大气输送的潜热通量和感热通量以及大气向海洋输送的动量通量等。结果表明:这次夏季风于5月21日从南海南部开始爆发,然后向北部扩展全面爆发。夏季风期间南海南部和南海北部的大气、海洋结构和海气交换特征等都有明显差别。此外,海表温度的变化除了与太阳总辐射有关外,主要是与海洋向大气输送的潜热通量变化有关,对本次夏季风发生较晚、强度较弱作了海-气交换的物理解释,并与1992~1993年西太平洋热带海域西风爆发过程作了比较。
根據1998年“南海季風試驗(SCSMEX)”彊化觀測期間“實驗3號”和“科學1號”科學攷察船船基大氣海洋自動觀測繫統兩點連續觀測的大氣、海洋資料,使用攷慮到風速和大氣層結影響的整體輸送公式計算海-氣間的湍流通量交換。根據計算結果分析南海夏季風期間海錶大氣要素和海溫日均值的逐日變化、海洋嚮大氣輸送的潛熱通量和感熱通量以及大氣嚮海洋輸送的動量通量等。結果錶明:這次夏季風于5月21日從南海南部開始爆髮,然後嚮北部擴展全麵爆髮。夏季風期間南海南部和南海北部的大氣、海洋結構和海氣交換特徵等都有明顯差彆。此外,海錶溫度的變化除瞭與太暘總輻射有關外,主要是與海洋嚮大氣輸送的潛熱通量變化有關,對本次夏季風髮生較晚、彊度較弱作瞭海-氣交換的物理解釋,併與1992~1993年西太平洋熱帶海域西風爆髮過程作瞭比較。
근거1998년“남해계풍시험(SCSMEX)”강화관측기간“실험3호”화“과학1호”과학고찰선선기대기해양자동관측계통량점련속관측적대기、해양자료,사용고필도풍속화대기층결영향적정체수송공식계산해-기간적단류통량교환。근거계산결과분석남해하계풍기간해표대기요소화해온일균치적축일변화、해양향대기수송적잠열통량화감열통량이급대기향해양수송적동량통량등。결과표명:저차하계풍우5월21일종남해남부개시폭발,연후향북부확전전면폭발。하계풍기간남해남부화남해북부적대기、해양결구화해기교환특정등도유명현차별。차외,해표온도적변화제료여태양총복사유관외,주요시여해양향대기수송적잠열통량변화유관,대본차하계풍발생교만、강도교약작료해-기교환적물리해석,병여1992~1993년서태평양열대해역서풍폭발과정작료비교。
Atmospheric and oceanic data collected by “Shiyan 3” and “Kexue 1” during the intensive observation period in SCSMEX98 were used to calculate the air-sea turbulent flux exchange. Here the calculation was based on the bulk aerodynamic formula, which had been considered the influence of wind speed and atmospheric stratification. Some characteristics of air-sea exchange were analyzed by examining the results. We found that the summer monsoon firstly burst out in the southern part of the South China Sea on May 21 and advanced northward to the whole. There were obvious differences in the characteristics of air-sea exchange between southern and northern. Moreover, the variation of SST mainly related to the latent flux transfer besides global radiation. We also gave an explanation for the later outbreak and weakness of the summer monsoon, and a comparison with westerly wind burst in the western equatorial Pacific Ocean from 1992 to 1993.