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Detailed Reference Information |
Shuman, C.A., Alley, R.B., Fahnestock, M.A., Fawcett, P.J., Bindschadler, R.A., White, J.W.C., Grootes, P.M., Anandakrishnan, S. and Stearns, C.R. (1997). Detection and monitoring of stratigraphic markers and temperature trends at the Greenland Ice Sheet Project 2 using passive-microwave remote-sensing data. Journal of Geophysical Research 102: doi: 10.1029/96JC02323. issn: 0148-0227. |
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Satellite passive-microwave sensors provide a sensitive means of studying ice-sheet surface processes that assists ice-core interpretation and can extend local observations across regional scales. Analysis of special sensor microwave/imager (SSM/I) brightness temperature (TB) data supports ice-core research in two specific ways. First, the summer hoar complex layers used to date the Holocene portion of the Greenland Ice Sheet Project 2 ice core can be defined temporally and spatially by SSM/I 37-GHz vertically (V) and horizontally (H) polarized B ratio (V/H) trends. Second, comparison of automatic weather station temperatures to SSM/I 37-GHz V TB data shows that they are an effective proxy temperature record in this region. Also, the TB data can be correlated with proxy temperature trends from stable-isotope-ratio (Δ18O and ΔD) profiles from snow pits and this allows the assignment of dates to specific snow depths. ¿ 1997 American Geophysical Union |
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Abstract |
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Keywords
Hydrology, Glaciology, Hydrology, Snow and ice, Meteorology and Atmospheric Dynamics, Climatology, Hydrology, Instruments and techniques |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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