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Titel Impact of congestus clouds on the midlevel ozone concentrations
VerfasserIn Toni Mitovski, Ian Folkins, Randall Martin, Matthew Cooper
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250046072
 
Zusammenfassung
We used simultaneous measurements from the TRMM 3B42 dataset and the SHADOZ ozonesonde network to identify high precipitation events and to construct height-time ozone anomaly patterns about Fiji and Samoa. The results clearly show an evidence of decreased (-10 ppbv) ozone concentrations in the middle troposphere (~ 6 km) preceding rainfall. Soundings from the IGRA dataset were used to calculate height-time divergence and RH anomaly patterns about high precipitation events. The results show that a mid-level divergence, likely due to congestus detrainment, is coincident with the mid-level ozone anomaly. An increased RH in the lower and middle troposphere, preceding peak rainfall, confirms presence of congestus clouds. The mid-level ozone and divergence anomaly features that precede rainfall are not seen in the GEOS-Chem model. The height, timing, and amplitude, of the mid-level congestus divergence, are not fully represented in the YOTC.