沙漠与绿洲气象
沙漠與綠洲氣象
사막여록주기상
DESERT AND OASIS METEOROLOGY
2012年
1期
1-9
,共9页
沙尘暴%蒙古气旋%诊断分析%高空急流
沙塵暴%矇古氣鏇%診斷分析%高空急流
사진폭%몽고기선%진단분석%고공급류
sand-dust storm%Mongolia cyclone%diagnosis and analysis%upper jet
利用卫星资料、加密观测资料、NCEP再分析资料分析了2009年4月下旬我国北方地区大范围沙尘天气过程的成因,并对热力、动力及不稳定层结等条件作了物理量诊断,得到了一些结果。贝加尔湖阻高、高空冷涡及蒙古气旋是造成此次大范围沙尘天气的有利环流形势,其中蒙古气旋是关键影响系统。干暖舌位置对于沙尘落区有一定指示意义,沙尘暴落区与干暖舌的位置及移动方向一致;沙尘天气主要发生在高空急流入口右侧,高空急流加强东移南压对应着沙尘天气东扩南压加强;螺旋度反映出沙尘暴过程中气旋区旋转上升明显,且螺旋度大值区后倾;理查逊数下降并维持低值、风垂直切变增大,大气层结不稳定,易激发沙尘暴发生和向下游传输。
利用衛星資料、加密觀測資料、NCEP再分析資料分析瞭2009年4月下旬我國北方地區大範圍沙塵天氣過程的成因,併對熱力、動力及不穩定層結等條件作瞭物理量診斷,得到瞭一些結果。貝加爾湖阻高、高空冷渦及矇古氣鏇是造成此次大範圍沙塵天氣的有利環流形勢,其中矇古氣鏇是關鍵影響繫統。榦暖舌位置對于沙塵落區有一定指示意義,沙塵暴落區與榦暖舌的位置及移動方嚮一緻;沙塵天氣主要髮生在高空急流入口右側,高空急流加彊東移南壓對應著沙塵天氣東擴南壓加彊;螺鏇度反映齣沙塵暴過程中氣鏇區鏇轉上升明顯,且螺鏇度大值區後傾;理查遜數下降併維持低值、風垂直切變增大,大氣層結不穩定,易激髮沙塵暴髮生和嚮下遊傳輸。
이용위성자료、가밀관측자료、NCEP재분석자료분석료2009년4월하순아국북방지구대범위사진천기과정적성인,병대열력、동력급불은정층결등조건작료물리량진단,득도료일사결과。패가이호조고、고공랭와급몽고기선시조성차차대범위사진천기적유리배류형세,기중몽고기선시관건영향계통。간난설위치대우사진락구유일정지시의의,사진폭락구여간난설적위치급이동방향일치;사진천기주요발생재고공급류입구우측,고공급류가강동이남압대응착사진천기동확남압가강;라선도반영출사진폭과정중기선구선전상승명현,차라선도대치구후경;리사손수하강병유지저치、풍수직절변증대,대기층결불은정,역격발사진폭발생화향하유전수。
In this paper, using the meteorological satellite data, the dense observation and NCEP/ NCAR re-analysis data, the cause of the large-scale sand-dust storm process over the north ofChina during late April 2009 was analyzed. The dynamic, thermodynamic and stratified unstable conditions of the process were diagnosed. Baikal blocking, high-level cold vortex and Mongolia cyclone were propitious for the dust-sand storm, and Mongolia cyclone was the key. Dry and warm tongue indicated the location of the area impacted by the dust-sand storm and the moving direction of the dust-sand storm. The development of upper jet flow was closely related to the dust storm. The storm weather mainly occurred in the right of inflow area of upper jet. With the jet moving southeastward and intensification, the sand-dust weather extended southeastward and enhanced. The helicity reflected the revolving and ascending in cyclone area during the process, and the high helicty area tilted backward. Richardson Number and vertical wind shear are important to sand-dust storm. It is easy to make for the occurring and transferring of sand-dust storm when Richardson Number declined and kept low value, vertical wind shear enlarged, and atmosphere was stratified unstable.