A Novel Framework to Study Trace Gas Transport in Deep Convective Clouds
Autor: | Radovan Krejci, Ilona Riipinen, Joel A. Thornton, Roman Bardakov, Annica M. L. Ekman, Julien Savre |
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Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
Convection
010504 meteorology & atmospheric sciences 010402 general chemistry Atmospheric sciences 01 natural sciences Physics::Geophysics Troposphere Deep convection trace gas transport lcsh:Oceanography Environmental Chemistry lcsh:GC1-1581 lcsh:Physical geography Astrophysics::Galaxy Astrophysics Physics::Atmospheric and Oceanic Physics 0105 earth and related environmental sciences Condensed Matter::Quantum Gases Global and Planetary Change Moisture large eddy simulation Method development deep convection 0104 chemical sciences Trace gas Aerosol General Earth and Planetary Sciences Environmental science method development lcsh:GB3-5030 aerosols Large eddy simulation |
Zdroj: | Journal of Advances in Modeling Earth Systems, Vol 12, Iss 5, Pp n/a-n/a (2020) |
ISSN: | 1942-2466 |
Popis: | Deep convective clouds reach the upper troposphere (8–15 km height). In addition to moisture and aerosol particles, they can bring aerosol precursor gases and other reactive trace gases from the planetary boundary layer to the cloud top. In this paper, we present a method to estimate trace gas transport based on the analysis of individual air parcel trajectories. Large eddy simulation of an idealized deep convective cloud was used to provide realistic environmental input to a parcel model. For a buoyant parcel, we found that the trace gas transport approximately follows one out of three scenarios, determined by a combination of the equilibrium vapor pressure (containing information about water‐solubility and pure component saturation vapor pressure) and the enthalpy of vaporization. In one extreme, the trace gas will eventually be completely removed by precipitation. In the other extreme, there is almost no vapor condensation on hydrometeors and most of the gas is transported to the top of the cloud. The scenario in between these two extremes is also characterized by strong gas condensation, but a small fraction of the trace gas may still be transported aloft. This approach confirms previously suggested patterns of inert trace gas behavior in deep convective clouds, agrees with observational data, and allows estimating transport in analytically simple and computationally efficient way compared to explicit cloud‐resolving model calculations. |
Databáze: | OpenAIRE |
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