Orographic Land-Atmosphere Interactions and the Diurnal Cycle of Low Level Clouds and Fog

Orographic Land-Atmosphere Interactions and the Diurnal Cycle of Low Level Clouds and Fog AbstractPrevious work illuminated landform controls on moisture convergence in the Southern Appalachian Mountains (SAM) promoting heterogeneity in the vertical structure of low level clouds (LLC) and seeder-feeder interactions (SFI) that significantly impact warm season precipitation. Here, the focus is on elucidating orographic land-atmosphere interactions associated with the observed diurnal cycle of LLC and fog in the region. Three distinct hydrometeorological regimes during the Integrated Precipitation and Hydrology Experiment (IPHEx) are examined using the Weather Research and Forecasting model. Sensitivity to the choice of planetary boundary layer parameterization was investigated in the light of IPHEx observations. Simulations using the MYNN (Mellor-Yamada-Nakanishi-Niino) scheme exhibit LLC and fog patterns most consistent with observations albeit without capturing SFI. Independently of synoptic regime, the simulations reveal two distinct modes of orographic controls on atmospheric moisture convergence patterns that explain the diurnal cycle of LLC and fog. First, a stationary nocturnal mode at meso-α scales associated with an extended flow separation zone supports low level pooling and trapping of cold, moist, stable air in the inner mountain on the lee side of the western topographic divide. Second, a dynamic daytime mode that results from the co-organization of ridge valley-circulations at the meso-γ scale and Rayleigh-Bénard convection at the meso-β scale is associated with widespread low level instability below the envelope orography. Orographic decoupling results in the formation of a shallow stagnation zone between the western and eastern topographic divides at night that contracts westward during daytime. Predominantly easterly and southeasterly low level moisture convergence patterns support early afternoon LLC formation in the inner SAM. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Journal of Hydrometeorology American Meteorological Society

Orographic Land-Atmosphere Interactions and the Diurnal Cycle of Low Level Clouds and Fog

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Publisher
American Meteorological Society
Copyright
Copyright © American Meteorological Society
ISSN
1525-7541
eISSN
1525-7541
D.O.I.
10.1175/JHM-D-16-0186.1
Publisher site
See Article on Publisher Site

Abstract

AbstractPrevious work illuminated landform controls on moisture convergence in the Southern Appalachian Mountains (SAM) promoting heterogeneity in the vertical structure of low level clouds (LLC) and seeder-feeder interactions (SFI) that significantly impact warm season precipitation. Here, the focus is on elucidating orographic land-atmosphere interactions associated with the observed diurnal cycle of LLC and fog in the region. Three distinct hydrometeorological regimes during the Integrated Precipitation and Hydrology Experiment (IPHEx) are examined using the Weather Research and Forecasting model. Sensitivity to the choice of planetary boundary layer parameterization was investigated in the light of IPHEx observations. Simulations using the MYNN (Mellor-Yamada-Nakanishi-Niino) scheme exhibit LLC and fog patterns most consistent with observations albeit without capturing SFI. Independently of synoptic regime, the simulations reveal two distinct modes of orographic controls on atmospheric moisture convergence patterns that explain the diurnal cycle of LLC and fog. First, a stationary nocturnal mode at meso-α scales associated with an extended flow separation zone supports low level pooling and trapping of cold, moist, stable air in the inner mountain on the lee side of the western topographic divide. Second, a dynamic daytime mode that results from the co-organization of ridge valley-circulations at the meso-γ scale and Rayleigh-Bénard convection at the meso-β scale is associated with widespread low level instability below the envelope orography. Orographic decoupling results in the formation of a shallow stagnation zone between the western and eastern topographic divides at night that contracts westward during daytime. Predominantly easterly and southeasterly low level moisture convergence patterns support early afternoon LLC formation in the inner SAM.

Journal

Journal of HydrometeorologyAmerican Meteorological Society

Published: Mar 8, 2017

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