气象
氣象
기상
METEOROLOGICAL MONTHLY
2009年
5期
66-73
,共8页
游庆龙%康世昌%李潮流%张强弓%李茂善%刘景时
遊慶龍%康世昌%李潮流%張彊弓%李茂善%劉景時
유경룡%강세창%리조류%장강궁%리무선%류경시
NCEP/NCAR再分析资料%实测气象资料%纳木错
NCEP/NCAR再分析資料%實測氣象資料%納木錯
NCEP/NCAR재분석자료%실측기상자료%납목착
NCEP/NCAR reanalysis%observational data%Nam Co
利用中国科学院青藏高原研究所纳木错多圈层综合观测研究站在念青唐古拉峰扎当冰川垭口(30.47°N、90.65°E,5800m)和纳木错站(30.77°N、90.99°E,4730m)的逐日平均气温、相对湿度、气压等资料,与同期NCEP/NCAR再分析资料进行了对比分析,讨论了再分析资料在纳木错流域湖泊/冰川区气候变化研究中的适用性.结果表明:扎当冰川垭口和纳木错站气压再分析资料的可信度好于气温,相对湿度稍差:扎当冰川垭口气压和相对湿度再分析值与实测值的差值在冬季偏大,夏季偏小,气温则相反.在研究期间,总体上再分析资料在冰川区的可信度好于湖泊区,再分析资料能很好地反映该地区地面气压、气温和相对湿度的日变化特征,在应用到该地区气候变化的研究时应考虑地形的影响.
利用中國科學院青藏高原研究所納木錯多圈層綜閤觀測研究站在唸青唐古拉峰扎噹冰川埡口(30.47°N、90.65°E,5800m)和納木錯站(30.77°N、90.99°E,4730m)的逐日平均氣溫、相對濕度、氣壓等資料,與同期NCEP/NCAR再分析資料進行瞭對比分析,討論瞭再分析資料在納木錯流域湖泊/冰川區氣候變化研究中的適用性.結果錶明:扎噹冰川埡口和納木錯站氣壓再分析資料的可信度好于氣溫,相對濕度稍差:扎噹冰川埡口氣壓和相對濕度再分析值與實測值的差值在鼕季偏大,夏季偏小,氣溫則相反.在研究期間,總體上再分析資料在冰川區的可信度好于湖泊區,再分析資料能很好地反映該地區地麵氣壓、氣溫和相對濕度的日變化特徵,在應用到該地區氣候變化的研究時應攷慮地形的影響.
이용중국과학원청장고원연구소납목착다권층종합관측연구참재념청당고랍봉찰당빙천오구(30.47°N、90.65°E,5800m)화납목착참(30.77°N、90.99°E,4730m)적축일평균기온、상대습도、기압등자료,여동기NCEP/NCAR재분석자료진행료대비분석,토론료재분석자료재납목착류역호박/빙천구기후변화연구중적괄용성.결과표명:찰당빙천오구화납목착참기압재분석자료적가신도호우기온,상대습도초차:찰당빙천오구기압화상대습도재분석치여실측치적차치재동계편대,하계편소,기온칙상반.재연구기간,총체상재분석자료재빙천구적가신도호우호박구,재분석자료능흔호지반영해지구지면기압、기온화상대습도적일변화특정,재응용도해지구기후변화적연구시응고필지형적영향.
In order to understand the reliability of NCEP/NCAR reanalysis data in the lake and glacier area in the Tibetan Plateau (TP), the observational data from the Col of Zhadang Glacier (30.47°N、U90. 65°E, 5800m) and Nam Co Station (30. 77°N、90. 99°E, 4730m) were compared with the reanalysis data from the National Centers of Environmental Prediction/National Centers for Atmospheric Research (NCEP/NCAR) during the same period. The reanalysis data can capture much of the synoptic-scale variability in daily mean pressure, temperature and relative humidity. Among them, the reanalyzed pressure is more confident than temperature and relative humidity at the Col of Zhadang Glacier and Nam Co Station. Differences between the reanalyzed and observational daily mean pressure and relative humidity are large in winter and less in summer, while differences between the reanalyzed and observational daily mean temperature are opposite. Reliability of reanalysis data is better at the Col of Zhadang Glacier than at Nam Co Station. The reanalyzed data can be used to study the trends of climate change in the glacier and lake area in the Nam Co Basin, and more attentions should be given to influences of topography.