
NSF Org: |
AGS Division of Atmospheric and Geospace Sciences |
Recipient: |
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Initial Amendment Date: | January 24, 2006 |
Latest Amendment Date: | January 24, 2006 |
Award Number: | 0540896 |
Award Instrument: | Interagency Agreement |
Program Manager: |
Bradley F. Smull
AGS Division of Atmospheric and Geospace Sciences GEO Directorate for Geosciences |
Start Date: | February 1, 2006 |
End Date: | January 31, 2009 (Estimated) |
Total Intended Award Amount: | $181,987.00 |
Total Awarded Amount to Date: | $181,987.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
181 WAINWRIGHT RD Annapolis MD US 21402-5008 (410)293-2504 |
Sponsor Congressional District: |
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Primary Place of Performance: |
181 WAINWRIGHT RD Annapolis MD US 21402-5008 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | Physical & Dynamic Meteorology |
Primary Program Source: |
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Program Reference Code(s): |
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Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
The scientific objective of this research is to use newly available spectral imaging techniques to quantify and thus better understand overcasts' visible features. Such improvements will create new observational criteria for testing the realism of atmospheric radiative transfer models of overcasts' visible-wavelength spectral structure.
The intellectual merit of the proposed research is that it would investigate overcasts in a fundamentally new way by complementing conventional spectroradiometry with high-resolution spectra extracted from digital images. This combination permits new kinds of analyses of overcasts' often rapidly changing features. Before now, studying the fine angular details of overcast radiance spectra has not been possible (and certainly not second-by-second), so the proposed research constitutes a wholly new method of atmospheric passive remote sensing. No comparable work exists for narrow field-of-view overcast radiances. The spectral structure of overcast radiances is useful in describing the spatial distribution of cloud optical depth and absorptivity. This in turn offers insights into details of the near-surface heat budget.
With suitable data inversion techniques, various atmospheric scattering models will be tested to see how well they account for a given overcast's visible structure, including details seen through linear polarizers. Currently, no detailed observational study of overcast polarization seems to exist. Such wide-ranging observations can provide valuable new insights into everyday phenomena that are now thought to be well understood both theoretically and phenomenologically.
The broader impacts of the study will be derived from benefits to science education and impacts on the general public. The digital imaging techniques developed for NSF-sponsored research will be translated into both daily classroom instruction and yearlong honors research projects for Naval Academy midshipmen. An improved understanding of the spatial and spectral distribution of overcast radiances has practical applications in many areas ranging from interior lighting and highway safety to plant growth and development. The principal investigator's presentations are apt to be a powerful recruiting tool for future atmospheric scientists and also for outreach to the general public.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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