热带海洋学报
熱帶海洋學報
열대해양학보
JOURNAL OF TROPICAL OCEANOGRAPHY
2015年
3期
36-47
,共12页
郭智亮%黎伟标%王磊%刘昊亚
郭智亮%黎偉標%王磊%劉昊亞
곽지량%려위표%왕뢰%류호아
热带扰动%热带气旋%南海%气旋生成
熱帶擾動%熱帶氣鏇%南海%氣鏇生成
열대우동%열대기선%남해%기선생성
tropical disturbance%tropical cyclone%South China Sea%cyclogenesis
热带扰动是热带地区重要的天气系统,可能有机会发展为热带气旋。文章利用卫星遥感和再分析资料对比了南海能够发展和不能够发展为热带气旋的热带扰动的特征差异。结果表明:南海发展和不发展热带扰动的时空分布具有显著的区域性和季节性;发展的热带扰动具有更慢的移动速度和更长的持续时间。比较热带扰动对应的气象因子,结果显示决定南海热带扰动能否发展的关键气象因子包括:850hPa相对涡度、垂直风切变、850hPa与500hPa大气温度差、向外长波辐射(OLR)和中层大气相对湿度,并且利用这些关键气象因子构建了判别南海热带扰动能否发展的预报方程。研究结果有助于提高我们对南海热带扰动发展和热带气旋生成的早期预报能力。
熱帶擾動是熱帶地區重要的天氣繫統,可能有機會髮展為熱帶氣鏇。文章利用衛星遙感和再分析資料對比瞭南海能夠髮展和不能夠髮展為熱帶氣鏇的熱帶擾動的特徵差異。結果錶明:南海髮展和不髮展熱帶擾動的時空分佈具有顯著的區域性和季節性;髮展的熱帶擾動具有更慢的移動速度和更長的持續時間。比較熱帶擾動對應的氣象因子,結果顯示決定南海熱帶擾動能否髮展的關鍵氣象因子包括:850hPa相對渦度、垂直風切變、850hPa與500hPa大氣溫度差、嚮外長波輻射(OLR)和中層大氣相對濕度,併且利用這些關鍵氣象因子構建瞭判彆南海熱帶擾動能否髮展的預報方程。研究結果有助于提高我們對南海熱帶擾動髮展和熱帶氣鏇生成的早期預報能力。
열대우동시열대지구중요적천기계통,가능유궤회발전위열대기선。문장이용위성요감화재분석자료대비료남해능구발전화불능구발전위열대기선적열대우동적특정차이。결과표명:남해발전화불발전열대우동적시공분포구유현저적구역성화계절성;발전적열대우동구유경만적이동속도화경장적지속시간。비교열대우동대응적기상인자,결과현시결정남해열대우동능부발전적관건기상인자포괄:850hPa상대와도、수직풍절변、850hPa여500hPa대기온도차、향외장파복사(OLR)화중층대기상대습도,병차이용저사관건기상인자구건료판별남해열대우동능부발전적예보방정。연구결과유조우제고아문대남해열대우동발전화열대기선생성적조기예보능력。
Tropical disturbances are part of the important weather systems in the tropical regions and have the potential to develop into tropical cyclones. In this study, the characteristics of developing and non-developing tropical disturbances over the South China Sea (SCS) were compared using satellite observations and reanalysis datasets. The results revealed that developing and non-developing tropical disturbances have significant regional and seasonal characteristics. The developing tropical disturbances have slower moving speeds and persist for a longer lifetime, compared with the non-developing tropical disturbances over the SCS. By investigating the meteorological variables for tropical disturbances over the SCS, five key environmental factors that could determine a tropical disturbance to develop or not are found, including the 850-hPa relative vorticity, vertical wind shear, the temperature difference between 850 and 500 hPa, the outgoing long wave radiation (OLR), and the mid-level atmospheric relative humidity. A forecasting equation has been developed based on these key meteorological factors to predict whether a tropical disturbance over the SCS will develop or not. These results can help us to better predict tropical disturbance development and tropical cyclone formation over the SCS.