FORECASTING OF CONVECTIVE ACTIVITY USING A ONE-DIMENSIONAL STEADY-STATE CLOUD MODEL

被引：0

作者：

ALEKSIC, N ^{[1
]}

NIKOLIC, I ^{[1
]}

JOVANOVIC, D ^{[1
]}

机构：

[1] REPUBL HYDROMETEOROL INST SERBIA, YU-11000 BELGRADE, YUGOSLAVIA

来源：

MONTHLY WEATHER REVIEW | 1991年 / 119卷 / 12期

关键词：

D O I：

10.1175/1520-0493(1991)119<3099:FOCAUA>2.0.CO;2

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

A steady-state one-dimensional cloud model is used for forecasts of maximum cloud-top heights, which are taken to be a measure of the strength of convective activity. The way the model is used as well as its verification based on radar observations is described. Results show that with a careful calibration the model produces acceptable results. Model performance is crucially dependent on the proper choice of boundary conditions. Boundary conditions should be seasonally dependent. However, separate calibrations for different weather conditions and mesoscale peculiarities are not necessary for reasonably good results.

引用

页码：3099 / 3103

页数：5

共 14 条

[1]

ACKERMAN B, 1985, J CLIM APPL METEOROL, V24, P617, DOI 10.1175/1520-0450(1985)024<0617:PBTODC>2.0.CO

[2]

[3] THE SUPERCOOLING OF WATER [J].

BIGG, EK .

PROCEEDINGS OF THE PHYSICAL SOCIETY OF LONDON SECTION B, 1953, 66 (404) :688-694

[4]

CRUM TD, 1983, MON WEATHER REV, V111, P829, DOI 10.1175/1520-0493(1983)111<0829:EISTFU>2.0.CO

[5]

[6]

ENGLISH M, 1975, J WEA MOD, V7, P43

[7]

HIRSCH J, 1971, PB281028AS

[8]

Orville H. D., 1973, Journal of Applied Meteorology, V12, P671, DOI 10.1175/1520-0450(1973)012<0671:OTFOLW>2.0.CO

[9]

[10]

ORVILLE HD, 1980, 8TH C WEATH FOR AN D, P247

← 1 2 →