大气科学学报
大氣科學學報
대기과학학보
JOURNAL OF NANJING INSTITUTE OF METEOROLOGY
2011年
5期
592-596
,共5页
汪玲玲%牛生杰%贾然%柯怡明%杨志彪%熊守权
汪玲玲%牛生傑%賈然%柯怡明%楊誌彪%熊守權
왕령령%우생걸%가연%가이명%양지표%웅수권
积雪%时空特征%环流背景%气象要素
積雪%時空特徵%環流揹景%氣象要素
적설%시공특정%배류배경%기상요소
snowcover%spatial and temporal characteristics%circulation background%meteorological factors
利用湖北省77个测站1961-2007年气象资料,分析了积雪的时空特征。结果表明,湖北省积雪年际变化振幅明显,20世纪60年代到70年代中期缓慢增加,为积雪多发期;80年代年波动较大;90年代开始明显减少。月积雪日数呈准正态分布,1月最多,2月、12月次之。积雪空间分布表现为西部多,中东部少;山地多,丘陵平原少;沿江多,内陆少。有利于湖北大范围出现积雪的大尺度背景的环流类型主要有纬向型和两槽一脊型。出现积雪时24h变压Δp24为正,24h变温Δt24和水汽压变化Δe24为负,地面气象要素的异常变化,也可以作为积雪预报的着眼点之一。
利用湖北省77箇測站1961-2007年氣象資料,分析瞭積雪的時空特徵。結果錶明,湖北省積雪年際變化振幅明顯,20世紀60年代到70年代中期緩慢增加,為積雪多髮期;80年代年波動較大;90年代開始明顯減少。月積雪日數呈準正態分佈,1月最多,2月、12月次之。積雪空間分佈錶現為西部多,中東部少;山地多,丘陵平原少;沿江多,內陸少。有利于湖北大範圍齣現積雪的大呎度揹景的環流類型主要有緯嚮型和兩槽一脊型。齣現積雪時24h變壓Δp24為正,24h變溫Δt24和水汽壓變化Δe24為負,地麵氣象要素的異常變化,也可以作為積雪預報的著眼點之一。
이용호북성77개측참1961-2007년기상자료,분석료적설적시공특정。결과표명,호북성적설년제변화진폭명현,20세기60년대도70년대중기완만증가,위적설다발기;80년대년파동교대;90년대개시명현감소。월적설일수정준정태분포,1월최다,2월、12월차지。적설공간분포표현위서부다,중동부소;산지다,구릉평원소;연강다,내륙소。유리우호북대범위출현적설적대척도배경적배류류형주요유위향형화량조일척형。출현적설시24h변압Δp24위정,24h변온Δt24화수기압변화Δe24위부,지면기상요소적이상변화,야가이작위적설예보적착안점지일。
Based on the meteorological data from 77 stations in Hubei Province from 1961 to 2007,the spatial and temporal distribution characteristics of snowcover were analyzed.Results show that the duration of annual snowcover days varies obviously.It increased from 1960s to the mid 1970s,which was the peak time of snowcover days.It fluctuated apparently in 1980s and decreased gradually from 1990s.The number of mensal snowcover days shows a quasi-normal distribution with a maximum value in January and then in February and December.Snowcover is more likely to occur in the west parts than in the middle and east,more likely to occur in mountains than on plains,and more likely to occur along the river than in midland.The two types of circulation background that is the most propitious for snowcover are zonal circulation or trough-ridge-trough.When snowcover occurs,Δp24 is positive and Δt24 and Δe24 are negative,which can be used to forecast snowcover by unwonted changes of meteorological factors.