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Monday, May 18, 2020 | History

3 edition of Identification and classification of transient signatures in over-land SSM/I imagery found in the catalog.

Identification and classification of transient signatures in over-land SSM/I imagery

Identification and classification of transient signatures in over-land SSM/I imagery

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  • 1 Currently reading

Published by National Aeronautics and Space Administration, National Technical Information Service, distributor in [Washington, DC, Springfield, Va .
Written in English

    Subjects:
  • Remote sensing.,
  • Detection.,
  • Surface temperature.,
  • Microwave imagery.,
  • Emissivity.,
  • Brightness temperature.

  • Edition Notes

    StatementGrant W. Petty, Mark D. Conner.
    Series[NASA contractor report] -- NASA-CR-202496., NASA contractor report -- NASA CR-202496.
    ContributionsConner, Mark D., United States. National Aeronautics and Space Administration.
    The Physical Object
    FormatMicroform
    Pagination1 v.
    ID Numbers
    Open LibraryOL15490361M

    6 Remotely Sensed Data Characterization, Classification, and Accuracies used to measure from a distance the amount of EMR exiting an aerial platforms, which are used by law enforcement and mili- object, or geographic area, then extracting valuable information tary 5/5(1). Present-day Antarctic Ice Mass Changes and Crustal Motion. NASA Technical Reports Server (NTRS) James, Thomas S.; Ivins, Erik R. The peak vertical velocities predicted by three realistic, but contrasting, present-day scenarios of Antarctic ice sheet mass balance are found to be of the order of several mm/a. One scenario predicts local uplift rates in excess of 5 mm/a.

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    Free essays, homework help, flashcards, research papers, book reports, term papers, history, science, politics. The different signatures might allow for discrimination of these different forcings; e.g., the warming of the s looks more like the altered ocean heat transport signal, while the warming of the s is more like the trace gas effect. quasi-stationary and transient. After 30 years of measurements by interplanetary spacecraft, the.


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Identification and classification of transient signatures in over-land SSM/I imagery Download PDF EPUB FB2

Get this from a library. Identification and classification of transient signatures in over-land SSM/I imagery. [Grant W Petty; Mark D Conner; United States. National Aeronautics and Space Administration.]. The spectral characteristics of brightness temperature measured by the Special Sensor Microwave/Imager (SSM/I) form the basis of a rain classification scheme (Grody, ), which is Author: Taifeng Yang.

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Barnett, T. P., An attempt to detect the greenhouse-gas signal in a transient GCM simulation. Greenhouse-Gas-Induced-Climatic Change: A Critical Appraisal of Simulations and Observations. Gridding. Use of a uniform system of rectilinear lines superimposed on imagery (such as photographs, mosaics, maps, charts, or other representations of the Earth’s surface).

Ground pattern. Any specific identifying feature of the land surface which can be used for classification purposes. WMOTDSatellite-Remote-Sensing-and-GIS-Applications-in-Agricultural-Meteorology. The Commission at that time noted that there was a demand in almost all countries for a capability to use satellite imagery in practical problems of agrometeorology.

Visible/IR Radiometer (VHRR) Microwave Radiometer (SSM/I, TMI, MSMR) Microwave. Bologna, Italy IV HyMeX Workshop June Book of Abstracts | 2 | P a g e Book of Abstracts Index Alphabetical Author Index.

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Figure (a and b) IR satellite imagery of Tropical Storm Georgette from UTC 27 Augustwith no enhancement in (a) and the standard BD Dvorak curve in (b). (c) SSM/I 85 GHz H pass from UTC over Georgette and (d) the composite image for the pass, illustrating the exposed low-level center located near N.

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% $Id$ % Purpose: Bibliographic database in BibTeX format % URL: % Usage: scp ~/tex/ :/var/www/html/doc. C. S. Ruf, A. S. S., J. Vongsathorn, and R. R. Ferraro, Determination of cloud liquid water content using the SSM/I flux estimation techniques, and fine-scale turbulence measurements in the unstable surface layer over land.

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