Estimation of the Impact of Gravity Heterogeneities on the Heat Regime of the Boundary Layer of the Atmosphere
Abstract The heterogeneities of the gravity field (HGF) deform the fields of air pressure, density, and temperature and affect the temperature regime of the boundary layer of the atmosphere, as well as the heat exchange between the air and the underlying surface. This work considers a stationary ana...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ingel, L. Kh. [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2021 |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2021. ISSN 1028-334X, Doklady Earth Sciences, 2021, Vol. 500, Part 1, pp. 777–780. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Doklady Rossiiskoi Akademii Nauk. Nauki o Zemle, 2021, Vol. 500, No. 1, pp. 83–87. |
|---|
| Übergeordnetes Werk: |
Enthalten in: Doklady earth sciences - Pleiades Publishing, 1998, 500(2021), 1 vom: Sept., Seite 777-780 |
|---|---|
| Übergeordnetes Werk: |
volume:500 ; year:2021 ; number:1 ; month:09 ; pages:777-780 |
| Links: |
|---|
| DOI / URN: |
10.1134/S1028334X21090117 |
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OLC2127939204 |
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| 520 | |a Abstract The heterogeneities of the gravity field (HGF) deform the fields of air pressure, density, and temperature and affect the temperature regime of the boundary layer of the atmosphere, as well as the heat exchange between the air and the underlying surface. This work considers a stationary analytical model intended for estimation of the amplitudes of these effects, which resulted in analytical equations for profiles of temperature disturbances and amplitudes of deviations of the vertical heat fluxes on the surfaces. In addition to the amplitudes of the HGF, the latter most strongly depend on the ambient background stratification. In highly anomalous regions, the amplitudes of deviations of heat fluxes can reach and exceed 1 W/$ m^{2} $, which gives grounds to take into account the HGF in climate calculations and numerical models of the atmosphere. | ||
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Ingel, L. Kh. |
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| title_sort |
estimation of the impact of gravity heterogeneities on the heat regime of the boundary layer of the atmosphere |
| title_auth |
Estimation of the Impact of Gravity Heterogeneities on the Heat Regime of the Boundary Layer of the Atmosphere |
| abstract |
Abstract The heterogeneities of the gravity field (HGF) deform the fields of air pressure, density, and temperature and affect the temperature regime of the boundary layer of the atmosphere, as well as the heat exchange between the air and the underlying surface. This work considers a stationary analytical model intended for estimation of the amplitudes of these effects, which resulted in analytical equations for profiles of temperature disturbances and amplitudes of deviations of the vertical heat fluxes on the surfaces. In addition to the amplitudes of the HGF, the latter most strongly depend on the ambient background stratification. In highly anomalous regions, the amplitudes of deviations of heat fluxes can reach and exceed 1 W/$ m^{2} $, which gives grounds to take into account the HGF in climate calculations and numerical models of the atmosphere. © Pleiades Publishing, Ltd. 2021. ISSN 1028-334X, Doklady Earth Sciences, 2021, Vol. 500, Part 1, pp. 777–780. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Doklady Rossiiskoi Akademii Nauk. Nauki o Zemle, 2021, Vol. 500, No. 1, pp. 83–87. |
| abstractGer |
Abstract The heterogeneities of the gravity field (HGF) deform the fields of air pressure, density, and temperature and affect the temperature regime of the boundary layer of the atmosphere, as well as the heat exchange between the air and the underlying surface. This work considers a stationary analytical model intended for estimation of the amplitudes of these effects, which resulted in analytical equations for profiles of temperature disturbances and amplitudes of deviations of the vertical heat fluxes on the surfaces. In addition to the amplitudes of the HGF, the latter most strongly depend on the ambient background stratification. In highly anomalous regions, the amplitudes of deviations of heat fluxes can reach and exceed 1 W/$ m^{2} $, which gives grounds to take into account the HGF in climate calculations and numerical models of the atmosphere. © Pleiades Publishing, Ltd. 2021. ISSN 1028-334X, Doklady Earth Sciences, 2021, Vol. 500, Part 1, pp. 777–780. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Doklady Rossiiskoi Akademii Nauk. Nauki o Zemle, 2021, Vol. 500, No. 1, pp. 83–87. |
| abstract_unstemmed |
Abstract The heterogeneities of the gravity field (HGF) deform the fields of air pressure, density, and temperature and affect the temperature regime of the boundary layer of the atmosphere, as well as the heat exchange between the air and the underlying surface. This work considers a stationary analytical model intended for estimation of the amplitudes of these effects, which resulted in analytical equations for profiles of temperature disturbances and amplitudes of deviations of the vertical heat fluxes on the surfaces. In addition to the amplitudes of the HGF, the latter most strongly depend on the ambient background stratification. In highly anomalous regions, the amplitudes of deviations of heat fluxes can reach and exceed 1 W/$ m^{2} $, which gives grounds to take into account the HGF in climate calculations and numerical models of the atmosphere. © Pleiades Publishing, Ltd. 2021. ISSN 1028-334X, Doklady Earth Sciences, 2021, Vol. 500, Part 1, pp. 777–780. © Pleiades Publishing, Ltd., 2021. Russian Text © The Author(s), 2021, published in Doklady Rossiiskoi Akademii Nauk. Nauki o Zemle, 2021, Vol. 500, No. 1, pp. 83–87. |
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Estimation of the Impact of Gravity Heterogeneities on the Heat Regime of the Boundary Layer of the Atmosphere |
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https://doi.org/10.1134/S1028334X21090117 |
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Makosko, A. A. |
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