Atmospheric infrared backscattering profiles: interpretation of statistical and temporal properties
Advanced Search
Select up to three search categories and corresponding keywords using the fields to the right. Refer to the Help section for more detailed instructions.

Search our Collections & Repository

For very narrow results

When looking for a specific result

Best used for discovery & interchangable words

Recommended to be used in conjunction with other fields

Dates

to

Document Data
Library
People
Clear All
Clear All

For additional assistance using the Custom Query please check out our Help Page

The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles, guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the NOAA IR retains documents in their original published format to ensure public access to scientific information.
i

Atmospheric infrared backscattering profiles: interpretation of statistical and temporal properties

Filetype[PDF-140.43 MB]


Select the Download button to view the document
Please click the download button to view the document.
Atmospheric infrared backscattering profiles: interpretation of statistical and temporal properties

Details:

  • Personal Author:
  • Corporate Authors:
  • NOAA Program & Office:
  • Description:
    This work describes the design, implementation, and calibration of NOAA's coherent, pulsed, Doppler lidar. This lidar was used to acquire 252 high-quality, independent measurements of atmospheric backscattering profiles from 4 to 30 km altitude over Boulder, Colorado, at a wavelength of 10.6 pm between May 1981 and May 1983, a period that includes the injection and removal of debris from the El Chichon eruptions. Statistical analyses of the data set by computer show that atmospheric backscatter is approximately

    lognormally distributed for all but the lowest altitudes, and a theoretical explanation is offered for this property. Seasonally averaged profiles and altitudinally stacked, filtered time sequences show the volcanic cloud appearing in the stratosphere and falling

    through the tropopause into the troposphere at rates far higher than can be explained by gravitational settling alone. The dynamic process of tropopause folding is proposed as the dominant mechanism for the observed exchange of volcanic debris from the stratosphere to the troposphere. This hypothesis is supported by case studies of mid-tropospheric backscatter-enhancing events. Mie calculations and comparisons with other measurements show that vertically integrated backscatter is a good long-term measure of total atmospheric mass loading of volcanic debris. It is found that the time constant that characterizes debris removal is 208 days for the stratosphere and 60 days for the troposphere. No appreciable debris is removed before the volcanic cloud falls to 6 km altitude 420 days after the volcanic eruptions.

  • Keywords:
  • Series:
  • Document Type:
  • License:
  • Rights Information:
    CC0 Public Domain
  • Compliance:
    Library
  • Main Document Checksum:
  • Download URL:
  • File Type:

Supporting Files

  • No Additional Files
More +

You May Also Like

Checkout today's featured content at repository.library.noaa.gov

Version 3.27.1