Detection and Characterization of Ash plumes from Eyjafjallajokull with Satellite Lidar

Autor: Winker, D. M., Liu, Z., Omar, A. H., Tackett, J. L., Fairlie, T. D., Pelon, Jacques
Přispěvatelé: NASA Langley Research Center [Hampton] (LaRC), National Institute of Aerospace [Hampton] (NIA), Science Systems and Applications, Inc. [Hampton] (SSAI), SPACE - LATMOS, Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Jazyk: angličtina
Rok vydání: 2010
Předmět:
Zdroj: American Geophysical Union Fall Meeting 2010
American Geophysical Union Fall Meeting 2010, Dec 2010, San Francisco, United States. pp.abstract id. NH51D-05
Popis: International audience; The eruption of the Eyjafjallajokull volcano in April-May 2010 highlighted the ash-monitoring capabilities of a variety of sensors now in orbit and the benefits of making use of observations from multiple sensors. Dispersion of the volcanic ash across Europe and subsequent impacts on air traffic resulted in the adoption of safety guidelines on acceptable ash mass concentrations, placing new requirements on the plume transport models used to provide ash advisories. The CALIPSO satellite carries a two-wavelength polarization lidar and a three-band IR radiometer, operating since June 2006. Profiles of spectral and polarized lidar backscatter are used to identify volcanic ash. CALIPSO first detected ash on 15 April and observed the dispersion of the ash plume as it spread across Europe, providing unique observations complementary to passive satellite sensors and groundbased lidars. With a vertical resolution of 60 meters, CALIPSO provides detailed profiles of the vertical distribution of ash. With estimates of ash particle size, which can be obtained from IR observations, profiles of mass concentration can be derived. The observed plume heights and vertically resolved property retrievals can be used for testing the underlying physics of plume transport models and to refine eruption source parameters used in the models. In addition to the lidar, CALIPSO also carries a multiwavelength infrared imager, presenting possibilities for combined lidar-infrared detection and retrieval schemes. This presentation will illustrate capabilities of CALIPSO to identify and characterize the ash plume from Eyjafjallajokull.
Databáze: OpenAIRE