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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2016-01-01
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Series: | Atmospheric Chemistry and Physics |
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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 |
work_keys_str_mv |
AT tdinh effectofgravitywavetemperaturefluctuationsonhomogeneousicenucleationinthetropicaltropopauselayer AT apodglajen effectofgravitywavetemperaturefluctuationsonhomogeneousicenucleationinthetropicaltropopauselayer AT ahertzog effectofgravitywavetemperaturefluctuationsonhomogeneousicenucleationinthetropicaltropopauselayer AT blegras effectofgravitywavetemperaturefluctuationsonhomogeneousicenucleationinthetropicaltropopauselayer AT rplougonven effectofgravitywavetemperaturefluctuationsonhomogeneousicenucleationinthetropicaltropopauselayer |
_version_ |
1725565268812365824 |