Small-Scale Spatial Variation of the Nocturnal Wind Field

被引:0
|
作者
Mahrt, L. [1 ]
Belusic, D. [2 ]
Acevedo, O. [3 ]
机构
[1] Northwest Res Associates, 2171 NW Kari Pl, Corvallis, OR 97330 USA
[2] Swedish Meteorol & Hydrol Inst SMHI, S-60176 Norrkoping, Sweden
[3] Univ Fed Santa Maria, BR-97105900 Santa Maria, RS, Brazil
基金
美国国家科学基金会;
关键词
Local spatial variation; Nocturnal boundary layer; Stratified turbulence; Submeso; Topography; STABLE BOUNDARY-LAYER; LOW-LEVEL JET; LARGE-EDDY SIMULATIONS; SUBMESO MOTIONS; SURFACE FLUXES; INTERMITTENT TURBULENCE; KINETIC-ENERGY; FLOW; TEMPERATURE; VARIABILITY;
D O I
10.1007/s10546-021-00627-z
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
This study examines the spatial variability of the nocturnal wind field using eight networks of surface observations ranging in horizontal width from 500 m to 65 km. The wind field is partitioned into small-scale variability (submeso motions) and the spatially-averaged wind vector. The vector-averaged wind is analogous to the wind resolved by a numerical model, posed here in terms of the wind that is vector averaged over an observational network. The small-scale variability represents the unresolved subgrid (sub-network) variation estimated in terms of the spatial variation of the wind vector within the observational domain. The bulk formula for the spatially-averaged heat flux is modified to account for the subgrid variation of the wind field. Investigation of the spatial variability of the wind field is also motivated by the need to estimate the representativeness of observations of the wind vector at an individual measurement site with respect to the wind field over the surrounding landscape. The small-scale variability of the observed wind field is contrasted between the networks as a function of the spatially-averaged wind vector, stratification, size of the network, and the topography. A strong dependence on topography emerges in spite of different instrumentation, deployment strategy, and processing for each network. Even weak topography can be important. A better design for future observational networks is briefly discussed.
引用
收藏
页码:225 / 245
页数:21
相关论文
共 50 条
  • [1] Small-Scale Spatial Variation of the Nocturnal Wind Field
    L. Mahrt
    D. Belušić
    O. Acevedo
    [J]. Boundary-Layer Meteorology, 2021, 180 : 225 - 245
  • [2] Small-scale spatial variation of macrobenthic community structure
    Mannino, A
    Montagna, PA
    [J]. ESTUARIES, 1997, 20 (01): : 159 - 173
  • [3] Small-scale spatial variation of macrobenthic community structure
    Antonio Mannino
    Paul A. Montagna
    [J]. Estuaries, 1997, 20 : 159 - 173
  • [4] Small-scale spatial variation of selenium concentrations in chironomid larvae
    Malloy, JC
    Meade, ML
    Olsen, EW
    [J]. BULLETIN OF ENVIRONMENTAL CONTAMINATION AND TOXICOLOGY, 1999, 62 (02) : 122 - 129
  • [5] Small-Scale Spatial Variation of Selenium Concentrations in Chironomid Larvae
    J. C. Malloy
    M. L. Meade
    E. W. Olsen
    [J]. Bulletin of Environmental Contamination and Toxicology, 1999, 62 : 122 - 129
  • [6] Small-Scale Variability in the Nocturnal Boundary Layer
    L. Mahrt
    Lena Pfister
    Christoph K. Thomas
    [J]. Boundary-Layer Meteorology, 2020, 174 : 81 - 98
  • [7] Small-Scale Variability in the Nocturnal Boundary Layer
    Mahrt, L.
    Pfister, Lena
    Thomas, Christoph K.
    [J]. BOUNDARY-LAYER METEOROLOGY, 2020, 174 (01) : 81 - 98
  • [8] Small-scale spatial variation of inundation dynamics in a floodplain of the Pantanal (Brazil)
    Pierre Girard
    Ibraim Fantin-Cruz
    Simoni M. Loverde de Oliveira
    Stephen K. Hamilton
    [J]. Hydrobiologia, 2010, 638 : 223 - 233
  • [9] Small-scale spatial variation of inundation dynamics in a floodplain of the Pantanal (Brazil)
    Girard, Pierre
    Fantin-Cruz, Ibraim
    Loverde de Oliveira, Simoni M.
    Hamilton, Stephen K.
    [J]. HYDROBIOLOGIA, 2010, 638 (01) : 223 - 233
  • [10] Small-scale spatial variation of benthic algal assemblages in a peat bog
    Cerna, Katerina
    [J]. LIMNOLOGICA, 2010, 40 (04): : 315 - 321