Retrieval of optical depth and particle size distribution of tropospheric and stratospheric aerosols by means of sun photometry

Journal Article · Wed Jan 01 04:00:00 EST 1997 · IEEE Transactions on Geoscience and Remote Sensing

DOI:https://doi.org/10.1109/36.551945· OSTI ID:458267

Schmid, B; Maetzler, C; Kaempfer, N ^[1]; Heimo, A ^[2]

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1. Univ. of Bern (Switzerland). Inst. of Applied Physics
2. Swiss Meteorological Inst., Payerne (Switzerland)

Aerosol optical depth measurements by means of ground-based Sun photometry were made in Bern, Switzerland during two and a half years primarily to provide quantitative corrections for atmospheric effects in remotely sensed data in the visible and near-infrared spectral region. An investigation of the spatial variability of tropospheric aerosol was accomplished in the summer of 1994 in the Swiss Central Plain, a region often covered by a thick aerosol layer. Intercomparisons are made with two Sun photometers operated by the Swiss Meteorological Institute in Payerne and Davos. By means of an inversion technique, columnar particle size distributions were derived from the aerosol optical depth spectra. Effective radius, columnar surface area, and columnar mass were computed from the inversion results. Most of the spectra measured in Bern exhibit an Angstroem-law dependence. Consequently, the inverted size distributions are very close to power-law distributions. Data collected during a four month calibration campaign in fall 1993 at a high-mountain station in the Swiss Alps allowed the authors to study optical properties of stratospheric aerosol. The extinction spectra measured have shown to be still strongly influenced by remaining aerosol of the June 1991 volcanic eruptions of Mount Pinatubo. Inverted particle size distributions can be characterized by a broad monodisperse peak with a mode radius around 0.25 {micro}m. Both aerosol optical depths and effective radii had not yet returned to pre-eruption values. Comparison of retrieved aerosol optical depth, columnar surface area and mass, with the values derived from lidar observations performed in Garmisch-Partenkirchen, Southern-Germany, yielded good agreement.

• OSTI ID: 458267
• Journal Information: IEEE Transactions on Geoscience and Remote Sensing, Journal Name: IEEE Transactions on Geoscience and Remote Sensing Journal Issue: 1 Vol. 35; ISSN IGRSD2; ISSN 0196-2892
• Country of Publication: United States
• Language: English

Related Subjects

54 ENVIRONMENTAL SCIENCES
AEROSOL MONITORING
AIR POLLUTION
PHOTOMETRY
REMOTE SENSING
STRATOSPHERE
TROPOSPHERE
VOLCANIC GASES