大气科学学报
大氣科學學報
대기과학학보
JOURNAL OF NANJING INSTITUTE OF METEOROLOGY
2011年
5期
606-613
,共8页
杨素英%马建中%胡志晋%金莲姬%许潇锋%高蒙
楊素英%馬建中%鬍誌晉%金蓮姬%許瀟鋒%高矇
양소영%마건중%호지진%금련희%허소봉%고몽
气溶胶%混合状态%云微物理%云模式
氣溶膠%混閤狀態%雲微物理%雲模式
기용효%혼합상태%운미물리%운모식
aerosols%mixing state%cloud microphysics%cloud model
在UWyo单组分气溶胶的绝热气块分档云模式基础上,发展了多种化学组分气溶胶的绝热气块分档云模式。利用2006年春季华北地区地面气溶胶分级采样的离子成分分析数据和同时段高空气溶胶、云微物理飞机观测资料,研究了气溶胶混合状态对暖云微物理特征的影响。模拟结果表明,华北地区气溶胶内部混合比外部混合有利于增加云凝结核数浓度、降低气块水汽最大饱和比、增加云滴数浓度。气溶胶的混合状态不同,形成的云滴谱的特征差异较大,主要体现在云滴谱的平均尺度和峰值的突出程度;云滴谱相对离散度在0.3附近变化,且随着云滴数浓度的增加,云滴谱相对离散度呈现减小的趋势。气溶胶混合状态能够影响暖云微物理特征,从而影响大气辐射和降水过程,在天气和气候变化的研究中应予以关注。
在UWyo單組分氣溶膠的絕熱氣塊分檔雲模式基礎上,髮展瞭多種化學組分氣溶膠的絕熱氣塊分檔雲模式。利用2006年春季華北地區地麵氣溶膠分級採樣的離子成分分析數據和同時段高空氣溶膠、雲微物理飛機觀測資料,研究瞭氣溶膠混閤狀態對暖雲微物理特徵的影響。模擬結果錶明,華北地區氣溶膠內部混閤比外部混閤有利于增加雲凝結覈數濃度、降低氣塊水汽最大飽和比、增加雲滴數濃度。氣溶膠的混閤狀態不同,形成的雲滴譜的特徵差異較大,主要體現在雲滴譜的平均呎度和峰值的突齣程度;雲滴譜相對離散度在0.3附近變化,且隨著雲滴數濃度的增加,雲滴譜相對離散度呈現減小的趨勢。氣溶膠混閤狀態能夠影響暖雲微物理特徵,從而影響大氣輻射和降水過程,在天氣和氣候變化的研究中應予以關註。
재UWyo단조분기용효적절열기괴분당운모식기출상,발전료다충화학조분기용효적절열기괴분당운모식。이용2006년춘계화북지구지면기용효분급채양적리자성분분석수거화동시단고공기용효、운미물리비궤관측자료,연구료기용효혼합상태대난운미물리특정적영향。모의결과표명,화북지구기용효내부혼합비외부혼합유리우증가운응결핵수농도、강저기괴수기최대포화비、증가운적수농도。기용효적혼합상태불동,형성적운적보적특정차이교대,주요체현재운적보적평균척도화봉치적돌출정도;운적보상대리산도재0.3부근변화,차수착운적수농도적증가,운적보상대리산도정현감소적추세。기용효혼합상태능구영향난운미물리특정,종이영향대기복사화강수과정,재천기화기후변화적연구중응여이관주。
An adiabatic bin-sized cloud parcel model is developed by incorporating the multi-chemical-component(MCC) aerosol effects into the UWyo single-chemical-component(SCC) parcel model.The effects of aerosols mixing state on the warm cloud microphysics in North China are investigated by using the model based on the data of ion component analysis of ground aerosol grade sampling and the aerosol and cloud microphysics observation in high latitude in North China in spring 2006.It is found that in North China the aerosol internal mixing increases the CCN number concentration and the cloud droplet number concentration(CDNC) and decreases the maximum saturation ratio of water vapor in air parcel.It is also shown that the different aerosols mixing states in North China can affect the cloud droplet spectra(CDS) characteristics especially the CDS's average size and the peak value prominence degree;the relative dispersion value of CDS is near 0.3,and it decreases with increasing CDNC.It is indicated that aerosol mixing state can influence the microphysics of warm clouds,and thus affects atmospheric radiation and precipitation.This should attract more attentions in weather and climate change research in the future.