Waves in SKRIPS: WAVEWATCH III coupling implementation and a case study of Tropical Cyclone Mekunu

被引:4
作者
Sun, Rui [1 ]
Cobb, Alison [1 ]
Boas, Ana B. Villas [2 ]
Langodan, Sabique [3 ]
Subramanian, Aneesh C. [4 ]
Mazloff, Matthew R. [1 ]
Cornuelle, Bruce D. [1 ]
Miller, Arthur J. [1 ]
Pathak, Raju [3 ]
Hoteit, Ibrahim [3 ]
机构
[1] Scripps Inst Oceanog, La Jolla, CA 92037 USA
[2] Colorado Sch Mines, Dept Geophys, Golden, CO USA
[3] King Abdullah Univ Sci & Technol KAUST, Phys Sci & Engn Div, Thuwal, Saudi Arabia
[4] Univ Colorado Boulder, Dept Atmospher & Ocean Sci, Boulder, CO USA
基金
美国海洋和大气管理局; 美国国家科学基金会; 美国国家航空航天局;
关键词
UPPER OCEAN RESPONSE; LANGMUIR TURBULENCE; BULK PARAMETERIZATION; WIND STRESS; PART I; MODEL; TRANSPORT; IMPACT; INTENSITY; PROFILES;
D O I
10.5194/gmd-16-3435-2023
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In this work, we integrated the WAVEWATCH III model into the regional coupled model SKRIPS (Scripps-KAUST Regional Integrated Prediction System). The WAVEWATCH III model is implemented with flexibility, meaning the coupled system can run with or without the wave component. In our implementations, we considered the effect of Stokes drift, Langmuir turbulence, sea surface roughness, and wave-induced momentum fluxes. To demonstrate the impact of coupling we performed a case study using a series of coupled and uncoupled simulations of Tropical Cyclone Mekunu, which occurred in the Arabian Sea in May 2018. We examined the model skill in these simulations and further investigated the impact of Langmuir turbulence in the coupled system. Because of the chaotic nature of the atmosphere, we ran an ensemble of 20 members for each coupled and uncoupled experiment. We found that the characteristics of the tropical cyclone are not significantly different due to the effect of surface waves when using different parameterizations, but the coupled models better capture the minimum pressure and maximum wind speed compared with the benchmark stand-alone Weather Research and Forecasting (WRF) model. Moreover, in the region of the cold wake, when Langmuir turbulence is considered in the coupled system, the sea surface temperature is about 0.5 & LCIRC;C colder, and the mixed layer is about 20 m deeper. This indicates the ocean model is sensitive to the parameterization of Langmuir turbulence in the coupled simulations.
引用
收藏
页码:3435 / 3458
页数:24
相关论文
共 101 条
  • [11] Centurioni Luca, 2019, NCEI, DOI 10.25921/7ntx-z961
  • [12] Impact of downward longwave radiative deficits on Antarctic sea-ice extent predictability during the sea ice growth period
    Cerovecki, Ivana
    Sun, Rui
    Bromwich, David H.
    Zou, Xun
    Mazloff, Matthew R.
    Wang, Sheng-Hung
    [J]. ENVIRONMENTAL RESEARCH LETTERS, 2022, 17 (08)
  • [13] Charnock H, 1955, Q J ROY METEOR SOC, V81, P639, DOI DOI 10.1002/QJ.49708135027
  • [14] The HYCOM (HYbrid Coordinate Ocean Model) data assimilative system
    Chassignet, Eric P.
    Hurlburt, Harley E.
    Smedstad, Ole Martin
    Halliwell, George R.
    Hogan, Patrick J.
    Wallcraft, Alan J.
    Baraille, Remy
    Bleck, Rainer
    [J]. JOURNAL OF MARINE SYSTEMS, 2007, 65 (1-4) : 60 - 83
  • [15] The CBLAST-hurricane program and the next-generation fully coupled atmosphere-wave-ocean. Models for hurricane research and prediction
    Chen, Shuyi S.
    Price, James F.
    Zhao, Wei
    Donelan, Mark A.
    Walsh, Edward J.
    [J]. BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY, 2007, 88 (03) : 311 - 317
  • [16] Development of a two-way-coupled ocean-wave model: assessment on a global NEMO(v3.6)-WW3(v6.02) coupled configuration
    Couvelard, Xavier
    Lemarie, Florian
    Samson, Guillaume
    Redelsperger, Jean-Luc
    Ardhuin, Fabrice
    Benshila, Rachid
    Madec, Gurvan
    [J]. GEOSCIENTIFIC MODEL DEVELOPMENT, 2020, 13 (07) : 3067 - 3090
  • [17] RATIONAL MODEL FOR LANGMUIR CIRCULATIONS
    CRAIK, ADD
    LEIBOVICH, S
    [J]. JOURNAL OF FLUID MECHANICS, 1976, 73 (FEB10) : 401 - 426
  • [18] Croize-Fillon D., 2013, GLOBAL ALTIMETER SWH
  • [19] D I. M., 2018, EXTR SEV CYCL STORM
  • [20] Quantifying upper ocean turbulence driven by surface waves
    D'Asaro, E. A.
    Thomson, J.
    Shcherbina, A. Y.
    Harcourt, R. R.
    Cronin, M. F.
    Hemer, M. A.
    Fox-Kemper, B.
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2014, 41 (01) : 102 - 107