Challenges in Numerical Weather Prediction of the 10 August 2020 Midwestern Derecho: Examples from the FV3-LAM

被引:5
作者
Gallus, William A. [1 ]
Harrold, Michelle A. [2 ,3 ]
机构
[1] Iowa State Univ, Dept Geol & Atmospher Sci, Ames, IA 50011 USA
[2] Natl Ctr Atmospher Res, Res Applicat Lab, Boulder, CO USA
[3] Dev Testbed Ctr, Boulder, CO USA
基金
美国海洋和大气管理局; 美国国家科学基金会;
关键词
Convective storms; systems; Mesoscale forecasting; Numerical weather prediction; forecasting; Convective parameterization; MESOSCALE CONVECTIVE SYSTEMS; LOW-LEVEL MESOVORTICES; PART I; DYNAMICAL CORE; SQUALL LINES; BOW ECHOES; NCEP GFS; CLIMATOLOGY; GENESIS; MODEL;
D O I
10.1175/WAF-D-23-0019.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
A severe derecho impacted the Midwestern United States on 10 August 2020, causing over $12 billion (U.S. dollars) in damage, and producing peak winds estimated at 63 m s-1, with the worst impacts in Iowa. The event was not forecast well by operational forecasters, nor even by operational and quasi-operational convection-allowing models. In the present study, nine simulations are performed using the Limited Area Model version of the Finite-Volume-Cubed -Sphere model (FV3-LAM) with three horizontal grid spacings and two physics suites. In addition, when a prototype of the Rapid Refresh Forecast System (RRFS) physics is used, sensitivity tests are performed to examine the impact of using the Grell-Freitas (GF) convective scheme. Several unusual results are obtained. With both the RRFS (not using GF) and Global Forecast System (GFS) physics suites, simulations using relatively coarse 13-and 25-km horizontal grid spacing do a much better job of showing an organized convective system in Iowa during the daylight hours of 10 August than the 3-km grid spacing runs. In addition, the RRFS run with 25-km grid spacing becomes much worse when the GF convective scheme is used. The 3-km RRFS run that does not use the GF scheme develops spurious nocturnal convection the night be-fore the derecho, removing instability and preventing the derecho from being simulated at all. When GF is used, the spuri-ous storms are removed and an excellent forecast is obtained with an intense bowing echo, exceptionally strong cold pool, and roughly 50 m s-1 surface wind gusts.
引用
收藏
页码:1429 / 1445
页数:17
相关论文
共 68 条
  • [1] Alexander R., 2013, NCEPEMC M
  • [2] Derecho hazards in the United States
    Ashley, WS
    Mote, TL
    [J]. BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2005, 86 (11) : 1577 - +
  • [3] Bow Echo Mesovortices. Part I: Processes That Influence Their Damaging Potential
    Atkins, Nolan T.
    Laurent, Michael St.
    [J]. MONTHLY WEATHER REVIEW, 2009, 137 (05) : 1497 - 1513
  • [4] Benjamin S. G., 2009, 13 C INTEGRATED OBSE
  • [5] Bentley ML, 1998, B AM METEOROL SOC, V79, P2527, DOI 10.1175/1520-0477(1998)079<2527:ACODPM>2.0.CO
  • [6] 2
  • [7] A 15 yr climatology of derecho-producing mesoscale convective systems over the central and eastern United States
    Bentley, ML
    Sparks, JA
    [J]. CLIMATE RESEARCH, 2003, 24 (02) : 129 - 139
  • [8] A Limited Area Modeling Capability for the Finite-Volume Cubed-Sphere (FV3) Dynamical Core and Comparison With a Global Two-Way Nest
    Black, T. L.
    Abeles, J. A.
    Blake, B. T.
    Jovic, D.
    Rogers, E.
    Zhang, X.
    Aligo, E. A.
    Dawson, L. C.
    Lin, Y.
    Strobach, E.
    Shafran, P. C.
    Carley, J. R.
    [J]. JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, 2021, 13 (06)
  • [9] Bryan GH, 2000, B AM METEOROL SOC, V81, P1207, DOI 10.1175/1520-0477(2000)081<1287:MAITSS>2.3.CO
  • [10] 2