Enhanced response of a stably stratified two-layer atmosphere to low-level heating
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- Type
- article
- Published
- 1995-01-01
- Cited by
- 6
- References
- 20
- Access
- Open access
- OpenAlex
- https://openalex.org/W31985861
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:116531158
Keywords
Stratification (seeds), Mechanics, Surface layer, Dissipation, Mixed layer
References
- Atmosphere-Ocean Dynamics
- A preliminary study of atmospheric waves using radiosonde data
- Weakly Nonlinear Response of a Stably Stratified Atmosphere to Diabatic Forcing in a Uniform Flow
- Trapping of Low-Level Internal Gravity Waves
- Transient Dynamics of Airflow near a Local Heat Source.
- Response of a Stably Stratified Atmosphere to Low-Level Heating— An Application to the Heat Island Problem
- Enhanced response of an atmospheric flow to a line-type heat sink in the presence of a critical level
- Two-Dimensional Response of a Stably Stratified Shear Flow to Diabatic Heating.
- City size and the urban heat island
- The Dynamics of Wave-Induced Downslope Winds
- Experimental study of mountain lee—waves by means of satellite photographs and aircraft measurements
- Solitary waves in the atmosphere
- Linearized Calculations of Urban Heat Island Convection Effects
- Banded Convective Activity and Ducted Gravity Waves
- The addition of heat to a stratified airstream with application to the dynamics of orographic rain
- Theory of waves in the lee of mountains
- Effects of Diabatic Cooling in a Shear Flow with a Critical Level
- The Airflow over Mountains: Research 1958-1972
- Role of a Critical Level in a Shear Flow with Diabatic Forcing
- The Influence of Mountains on the Atmosphere
Cited by
- Gravity wave generation in the lower stratosphere due to passage of the typhoon 9426 (Orchid) observed by the MU radar at Shigaraki (34.85°N, 136.10°E)
- An overview of the past, present and future of gravity‐wave drag parametrization for numerical climate and weather prediction models
- Effects of boundary-layer stability on urban heat island-induced circulation
- Momentum Flux by Thermally Induced Internal Gravity Waves and Its Approximation for Large-Scale Models
- Orographic–convective flows, wave reflection, and gravity-wave momentum fluxes in a two-layer hydrostatic atmosphere
- Inversion breakup over different shapes of urban areas
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