SODAR OBSERVATIONS OF THE STABLE LOWER ATMOSPHERIC BOUNDARY-LAYER AT BARROW, ALASKA

被引：13

作者：

CHEUNG, TK ^{[1
]}

机构：

[1] NOAA,ENVIRONM RES LAB,BOULDER,CO 80303

来源：

BOUNDARY-LAYER METEOROLOGY | 1991年 / 57卷 / 03期

关键词：

D O I：

10.1007/BF00120887

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

Events in the stably stratified lower atmospheric boundary layer within the first several hundreds of meters at Barrow, Alaska were recorded from 27 March to 5 April 1990 using an acoustic sounder (sodar), a tethered balloon, radiosondes, and an instrumented meteorological tower. These events include ground-based and low-level inversion layers, gravity waves, breaking waves, and multiple-layer structures. Even though these events are commonly found in a stable boundary layer, it is perhaps surprising to find them in such a slowly changing environment and over a terrain that is essentially devoid of immediate orographic influence.

引用

页码：251 / 274

页数：24

共 36 条

[21]

Hooke W. H., 1973, Boundary-Layer Meteorology, V5, P29, DOI 10.1007/BF02188309

[22] CHARACTERISTICS OF THE LOW-LEVEL TEMPERATURE INVERSION ALONG THE ALASKAN ARCTIC COAST [J].