Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer

The impact of high-frequency fluctuations of temperature on homogeneous nucleation of ice crystals in the vicinity of the tropical tropopause is investigated using a bin microphysics scheme for air parcels. The imposed temperature fluctuations come from measurements during isopycnic balloon flig...

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Main Authors: T. Dinh, A. Podglajen, A. Hertzog, B. Legras, R. Plougonven
Format: Article
Language:English
Published: Copernicus Publications 2016-01-01
Series:Atmospheric Chemistry and Physics
Online Access:https://www.atmos-chem-phys.net/16/35/2016/acp-16-35-2016.pdf
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spelling doaj-72f52fc3a50544f6af2cd0acf99fc93c2020-11-24T23:23:07ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242016-01-0116354610.5194/acp-16-35-2016Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layerT. Dinh0A. Podglajen1A. Hertzog2B. Legras3R. Plougonven4Program in Atmospheric and Oceanic Sciences, Princeton University, Princeton, New Jersey, USALaboratoire de Météorologie Dynamique, École Polytechnique, Palaiseau, FranceLaboratoire de Météorologie Dynamique, École Polytechnique, Palaiseau, FranceLaboratoire de Météorologie Dynamique, École Normale Supérieure, Paris, FranceLaboratoire de Météorologie Dynamique, École Polytechnique, Palaiseau, FranceThe impact of high-frequency fluctuations of temperature on homogeneous nucleation of ice crystals in the vicinity of the tropical tropopause is investigated using a bin microphysics scheme for air parcels. The imposed temperature fluctuations come from measurements during isopycnic balloon flights near the tropical tropopause. The balloons collected data at high frequency, guaranteeing that gravity wave signals are well resolved.<br><br>With the observed temperature time series, the numerical simulations with homogeneous freezing show a full range of ice number concentration (INC) as previously observed in the tropical upper troposphere. In particular, a low INC may be obtained if the gravity wave perturbations produce a non-persistent cooling rate (even with large magnitude) such that the absolute change in temperature remains small during nucleation. This result is explained analytically by a dependence of the INC on the absolute drop in temperature (and not on the cooling rate). This work suggests that homogeneous ice nucleation is <span style="" class="text italic">not</span> necessarily inconsistent with observations of low INCs.</p>https://www.atmos-chem-phys.net/16/35/2016/acp-16-35-2016.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Dinh
A. Podglajen
A. Hertzog
B. Legras
R. Plougonven
spellingShingle T. Dinh
A. Podglajen
A. Hertzog
B. Legras
R. Plougonven
Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer
Atmospheric Chemistry and Physics
author_facet T. Dinh
A. Podglajen
A. Hertzog
B. Legras
R. Plougonven
author_sort T. Dinh
title Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer
title_short Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer
title_full Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer
title_fullStr Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer
title_full_unstemmed Effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer
title_sort effect of gravity wave temperature fluctuations on homogeneous ice nucleation in the tropical tropopause layer
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2016-01-01
description The impact of high-frequency fluctuations of temperature on homogeneous nucleation of ice crystals in the vicinity of the tropical tropopause is investigated using a bin microphysics scheme for air parcels. The imposed temperature fluctuations come from measurements during isopycnic balloon flights near the tropical tropopause. The balloons collected data at high frequency, guaranteeing that gravity wave signals are well resolved.<br><br>With the observed temperature time series, the numerical simulations with homogeneous freezing show a full range of ice number concentration (INC) as previously observed in the tropical upper troposphere. In particular, a low INC may be obtained if the gravity wave perturbations produce a non-persistent cooling rate (even with large magnitude) such that the absolute change in temperature remains small during nucleation. This result is explained analytically by a dependence of the INC on the absolute drop in temperature (and not on the cooling rate). This work suggests that homogeneous ice nucleation is <span style="" class="text italic">not</span> necessarily inconsistent with observations of low INCs.</p>
url https://www.atmos-chem-phys.net/16/35/2016/acp-16-35-2016.pdf
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