气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2013年
6期
42-48
,共7页
马明亮%申红艳%魏鸿业%张加昆
馬明亮%申紅豔%魏鴻業%張加昆
마명량%신홍염%위홍업%장가곤
河谷%复杂地形%逆温%环境风险
河穀%複雜地形%逆溫%環境風險
하곡%복잡지형%역온%배경풍험
Valley%Complex terrain%Inversion temperature%Environmental risk
利用中尺度气象模式模拟了特殊地形下的气象变化特征,通过 CALPUFF 模拟了大气环境风险事件的精细化扩散特征。结果表明:西宁市地面风特征与河谷地形走向基本一致,典型风场表现为湟水河谷盛行西北和东南风,北川河谷则多为偏北风。青藏高原昼间强烈的山坡辐射增热和夜间冷却效应致使低空出现逆温层频率高,全年逆温的频率约为36%,最高逆温强度达每百米增温2.0℃以上,不利于污染物在垂直方向的扩散,河谷剖面模拟温度场的结果显示相同高度山坡附近比河谷中心的温度大约高1.5℃。CALPUFF 在西宁市大气环境风险模拟结果中能清楚描绘出污染物沿河谷输送与扩散的初始状况和细致分布,同时出现山体对烟团的阻碍效应、烟团因流场在山脊处形变以及山谷风环流影响等非定常扩散现象,扩散轨迹符合复杂地形和气象条件影响的特征和规律,模拟结果对准确预估大气环境风险事件在复杂地形和气象条件下城市中的扩散特征、影响范围和程度具有重要意义。
利用中呎度氣象模式模擬瞭特殊地形下的氣象變化特徵,通過 CALPUFF 模擬瞭大氣環境風險事件的精細化擴散特徵。結果錶明:西寧市地麵風特徵與河穀地形走嚮基本一緻,典型風場錶現為湟水河穀盛行西北和東南風,北川河穀則多為偏北風。青藏高原晝間彊烈的山坡輻射增熱和夜間冷卻效應緻使低空齣現逆溫層頻率高,全年逆溫的頻率約為36%,最高逆溫彊度達每百米增溫2.0℃以上,不利于汙染物在垂直方嚮的擴散,河穀剖麵模擬溫度場的結果顯示相同高度山坡附近比河穀中心的溫度大約高1.5℃。CALPUFF 在西寧市大氣環境風險模擬結果中能清楚描繪齣汙染物沿河穀輸送與擴散的初始狀況和細緻分佈,同時齣現山體對煙糰的阻礙效應、煙糰因流場在山脊處形變以及山穀風環流影響等非定常擴散現象,擴散軌跡符閤複雜地形和氣象條件影響的特徵和規律,模擬結果對準確預估大氣環境風險事件在複雜地形和氣象條件下城市中的擴散特徵、影響範圍和程度具有重要意義。
이용중척도기상모식모의료특수지형하적기상변화특정,통과 CALPUFF 모의료대기배경풍험사건적정세화확산특정。결과표명:서저시지면풍특정여하곡지형주향기본일치,전형풍장표현위황수하곡성행서북화동남풍,북천하곡칙다위편북풍。청장고원주간강렬적산파복사증열화야간냉각효응치사저공출현역온층빈솔고,전년역온적빈솔약위36%,최고역온강도체매백미증온2.0℃이상,불리우오염물재수직방향적확산,하곡부면모의온도장적결과현시상동고도산파부근비하곡중심적온도대약고1.5℃。CALPUFF 재서저시대기배경풍험모의결과중능청초묘회출오염물연하곡수송여확산적초시상황화세치분포,동시출현산체대연단적조애효응、연단인류장재산척처형변이급산곡풍배류영향등비정상확산현상,확산궤적부합복잡지형화기상조건영향적특정화규률,모의결과대준학예고대기배경풍험사건재복잡지형화기상조건하성시중적확산특정、영향범위화정도구유중요의의。
The meteorological elements under special terrain were simulated by a mecoscale numerical model,and the fine diffusion characteristics for an atmospheric environment risk event were simulated by the CALPUFF mod-el.The results show that surface wind direction is parallel to the valley direction.The west-north and east-south wind and north wind prevail in Huangshui river valley and in Beichuan river valley,respectively.Strongly hillside daytime radiative heating and night cooling effect in Qinghai-Tibet plateau lead to inversion layer frequently with high intensity,and the frequency of inversion temperature reaches 36%,while the maximum intensity increases 2.0 ℃ every the 100 m height,which is not favorable to diffuse pollutants in vertical direction.By simulation,tem-perature in same height hillside is about 1.5 ℃ higher than in the center of valley.CALPUFF plume trajectory model can be applied to the simulation of atmospheric environmental risk events,and the simulation results clearly depict the initial condition and detailed distribution about pollutant transport and diffusion along the valley.Under the complex terrain and weather conditions,some diffusion phenomena will appear such as puff is hindered by the mountain,puff diffusion locus accords to the characteristic and regulation from stream affection and puff diffusion is influenced by circulation of valley wind,which have important significance to estimate the diffusion,influencing range and extent for atmospheric environmental risks in the city.