Statistical analysis of ice microphysical properties in tropical mesoscale convective systems derived from cloud radar and in situ microphysical observations
Autor: | Julien Delanoë, John W. Strapp, Delphine Leroy, Lyle Lilie, Fabien Dezitter, Alfons Schwarzenboeck, Emmanuel Fontaine, Alain Protat |
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Přispěvatelé: | Department of Atmospheric Sciences [Taoyuan City], National Central University [Taiwan] (NCU), Laboratoire de Météorologie Physique (LaMP), Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA), SPACE - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Centre for Australian Weather and Climate Research (CAWCR), Airbus [France], Met Analytics Inc. [Toronto], Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS) |
Jazyk: | angličtina |
Rok vydání: | 2020 |
Předmět: |
In situ
Convection [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] 020301 aerospace & aeronautics Atmospheric Science Cloud radar 010504 meteorology & atmospheric sciences Meteorology Mesoscale meteorology 02 engineering and technology Numerical weather prediction 01 natural sciences lcsh:QC1-999 Crystal lcsh:Chemistry Altitude 0203 mechanical engineering lcsh:QD1-999 13. Climate action Extinction (optical mineralogy) Environmental science lcsh:Physics 0105 earth and related environmental sciences |
Zdroj: | Atmospheric Chemistry and Physics Atmospheric Chemistry and Physics, 2020, 20 (6), pp.3503-3553. ⟨10.5194/acp-20-3503-2020⟩ Atmospheric Chemistry and Physics, Vol 20, Pp 3503-3553 (2020) Atmospheric Chemistry and Physics, European Geosciences Union, 2020, 20 (6), pp.3503-3553. ⟨10.5194/acp-20-3503-2020⟩ |
ISSN: | 1680-7316 1680-7324 |
DOI: | 10.5194/acp-20-3503-2020⟩ |
Popis: | This study presents a statistical analysis of the properties of ice hydrometeors in tropical mesoscale convective systems observed during four different aircraft campaigns. Among the instruments on board the aircraft, we focus on the synergy of a 94 GHz cloud radar and two optical array probes (OAP; measuring hydrometeor sizes from 10 µm to about 1 cm). For two campaigns, an accurate simultaneous measurement of the ice water content is available, while for the two others, ice water content is retrieved from the synergy of the radar reflectivity measurements and hydrometeor size and morphological retrievals from OAP probes. The statistics of ice hydrometeor properties are calculated as a function of radar reflectivity factor measurement percentiles and temperature. Hence, mesoscale convective systems (MCS) microphysical properties (ice water content, visible extinction, mass–size relationship coefficients, total concentrations, and second and third moments of hydrometeor size distribution) are sorted in temperature (and thus altitude) zones, and each individual campaign is subsequently analyzed with respect to median microphysical properties of the merged dataset (merging all four campaign datasets). The study demonstrates that ice water content (IWC), visible extinction, total crystal concentration, and the second and third moments of hydrometeor size distributions are similar in all four types of MCS for IWC larger than 0.1 g m−3. Finally, two parameterizations are developed for deep convective systems. The first concerns the calculation of the visible extinction as a function of temperature and ice water content. The second concerns the calculation of hydrometeor size distributions as a function of ice water content and temperature that can be used in numerical weather prediction. |
Databáze: | OpenAIRE |
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