THE HELSINKI TESTBED A Mesoscale Measurement, Research, and Service Platform

被引：44

作者：

Koskinen, Jarkko T. ^{[1
]}

Poutiainen, Jani ^{[1
]}

Schultz, David M. ^{[1
,2
,5
]}

Joffre, Sylvain ^{[1
]}

Koistinen, Jarmo ^{[1
]}

Saltikoff, Elena ^{[1
]}

Gregow, Erik ^{[1
]}

Turtiainen, Heikki ^{[4
]}

Dabberdt, Walter F. ^{[3
]}

Damski, Juhani ^{[1
]}

Eresmaa, Noora ^{[1
]}

Goke, Sabine ^{[2
]}

Hyvarinen, Otto ^{[1
]}

Jarvi, Leena ^{[2
,6
]}

Karppinen, Ari ^{[1
]}

Kotro, Janne ^{[1
]}

Kuitunen, Timo ^{[1
]}

Kukkonen, Jaakko ^{[1
]}

Kulmala, Markku ^{[2
]}

Moisseev, Dmitri ^{[2
]}

Nurmi, Pertti ^{[1
]}

Pohjola, Heikki ^{[4
]}

Pylkko, Pirkko ^{[1
]}

Vesala, Timo ^{[2
]}

Viisanen, Yrjo ^{[1
]}

机构：

[1] Finnish Meteorol Inst, FI-00101 Helsinki, Finland

[2] Univ Helsinki, Dept Phys, Div Atmospher Sci, Helsinki, Finland

[3] Vaisala Inc, Boulder, CO USA

[4] Vaisala Oyj, Vantaa, Finland

[5] Univ Manchester, Sch Earth Atmospher & Environm Sci, Ctr Atmospher Sci, Manchester, Lancs, England

[6] Kings Coll London, Dept Geog, London WC2R 2LS, England

来源：

BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY | 2011年 / 92卷 / 03期

基金：

芬兰科学院;

关键词：

SURFACE-ATMOSPHERE INTERACTIONS; MIXING HEIGHT DETERMINATION; ENTRAINMENT ZONE THICKNESS; IN-SITU VERIFICATION; MIXED-LAYER DEPTH; CO2; FLUXES; HYDROMETEOR CLASSIFICATION; METEOROLOGICAL INFORMATION; RADAR MEASUREMENTS; SOUTHERN FINLAND;

D O I：

10.1175/2010BAMS2878.1

中图分类号：

P4 [大气科学（气象学）];

学科分类号：

0706 ; 070601 ;

摘要：

The Helsinki Testbed is an open research and quasi-operational program designed to advance observing systems and strategies, understanding of mesoscale weather phenomena, urban and regional modeling, and applications in a high-latitude coastal environment. The skeleton of the Helsinki Testbed network was established from the existing observation networks of FMI and the Finnish Road Administration. The term nowcasting refers to shortrange forecasts primarily for the next two hours. On this time scale, weather information is mainly based on observations and rather simple extrapolations of past and present weather. Real-time data were made publicly available, and intense measurements were performed during five specific monthlong measurement campaigns between August 2005 and August 2006. Stable boundary layers frequently occur in the cool season and are a challenge for adequately describing the boundary layer in numerical weather prediction (NWP) and air quality models.

引用

页码：325 / 342

页数：18

共 67 条

[1] [Anonymous], 1987, BOUNDARY LAYER CLIMA
[2] [Anonymous], 22 C WEATH AN FOR 18
[3] [Anonymous], 2009, OBS WEATH CLIM GROUN
[4] [Anonymous], FAIR WEATH EFF PARTN
[5] Benjamin SG, 2004, MON WEATHER REV, V132, P495, DOI 10.1175/1520-0493(2004)132<0495:AHACTR>2.0.CO
[6] 2
[7] Benjamin SG, 2004, MON WEATHER REV, V132, P473, DOI 10.1175/1520-0493(2004)132<0473:MWPWTR>2.0.CO
[8] 2
[9] Bozier K. E., 2007, Weather, V62, P203, DOI 10.1002/wea.48
[10] Capsoni C, 2001, J ATMOS OCEAN TECH, V18, P609, DOI 10.1175/1520-0426(2001)018<0609:SCOPAO>2.0.CO

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