Autor: | S. Godin, Y. Emery, G. Megie, C. Flesia, Christine David |
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Rok vydání: | 1997 |
Předmět: |
Atmospheric Science
010504 meteorology & atmospheric sciences 010502 geochemistry & geophysics Atmospheric sciences 01 natural sciences Lidar Arctic 13. Climate action Phase (matter) Synoptic scale meteorology Thermal Frost Depolarization ratio Environmental Chemistry Environmental science Polar 0105 earth and related environmental sciences |
Zdroj: | Journal of Atmospheric Chemistry. 27:1-16 |
ISSN: | 0167-7764 |
DOI: | 10.1023/a:1005820407467 |
Popis: | The airborne lidar LEANDRE was deployed from Kiruna (Sweden) in January1995, during Phase III of the Second European Stratospheric Arctic andMid-latitude Experiment (SESAME). Polar Stratospheric Clouds (PSC) weredetected on several flights. Four lidar retrievals, on two different days, arepresented together with the thermal history of air masses, derived from 5-daybackward trajectories calculated from the TOPCAT model, using ECMWF analyses.The first PSC case was observed at the synoptic scale and at a temperatureclose to the ice frost point, with no significant depolarization, suggestingthat particles were in the liquid phase, probably liquid ternaryH2SO4/HNO3/H2Osolution forming a Type 1b cloud. Locally, on the same day, a Type II PSC (icecloud) was detected above the Scandinavian Mountains and was related tomesoscale processes. On another day, the third lidar retrieval only showedbackground aerosols signature, whereas the last one was performed at the NATequilibrium temperature and its measured depolarization ratio was consistentwith few solid state Type Ia particles, probably composed of NAT. From thethermal histories, the different behaviour of the two Type I clouds isexplained in terms of cooling rates and compositional hysteresis, driven bytemperature. |
Databáze: | OpenAIRE |
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