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Wind Fields over the Great Lakes Measured by the SeaWinds Scatterometer on the QuikSCAT Satellite
Affiliation:1. Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, MS 300-235, Pasadena, California 91107;2. National Oceanic and Atmospheric Administration, Great Lakes Environmental Research Laboratory, 2205 Commonwealth Blvd. Ann Arbor, Michigan 48105;2. LANXESS Deutschland GmbH, 50569 Köln, Germany;1. Institute for Molecular Biology, Hannover Medical School, Carl- Neuberg Str.1, D-30625 Hannover, Germany;2. Department of Gastroenterology, Hepatology, and Endocrinology, Hannover Medical School, Carl- Neuberg Str.1, D-30625 Hannover, Germany;3. German Center for Infection Research (DZIF), Braunschweig-Hannover site, Germany;4. Institute of Virology, Hannover Medical School, Carl- Neuberg Str.1, D-30625 Hannover, Germany;5. Institute of Virology, University Hospital Essen, University of Duisburg- Essen, D-45147 Essen, Germany;1. School of Chemical Sciences, North Maharashtra University, Jalgaon, MS, India;2. Department of Applied Chemistry, SV National Institute Technology, Surat, Gujarat, India;3. Department of Chemistry, Indian Institute Technology, Ropar, Punjab, India;4. Department of Chemistry, G.T. Patil College, Nandurbar, Maharashtra, India;1. State Key Laboratory of Information Engineering in Surveying, Mapping and Remote Sensing, Wuhan University, Wuhan, Hubei Province, China;2. Collaborative Innovation Center for Geospatial Technology, Wuhan, Hubei Province, China;3. Hubei Provincial Meteorological Bureau, Wuhan, Hubei Province, China;1. Forest Products Technology and Timber Construction Department, Salzburg University of Applied Sciences, Markt 136a, 5431, Kuchl, Austria;2. University of Transilvania in Brasov, B-dul Eroilor nr. 29, 500306, Brasov, Romania
Abstract:This paper demonstrates the utility of satellite scatterometer measurements for wind retrieval over the Great Lakes on a daily basis. We use data acquired by the SeaWinds Scatterometer on the QuikSCAT (QSCAT) satellite launched in June 1999 to derive wind speeds and directions over the lakes at a resolution of 12.5 km, which is two times finer than the QSCAT standard ocean wind product at a resolution of 25 km. To evaluate QSCAT performance for high-resolution measurements of lake wind vectors, we compare QSCAT results with Great Lakes Coastal Forecasting System (GLCFS) nowcast wind fields and with standard QSCAT measurements of ocean wind vectors. Although the satellite results over the Great Lakes are obtained with an ocean model function, QSCAT and GLCFS wind fields compare well together for low to moderate wind conditions (4–32 knots). For wind speed, the analysis shows a correlation coefficient of 0.71, a bias of 2.6 knots in mean wind speed difference (nowcast wind is lower) with a root-mean-square (rms) deviation of 3.8 knots. For wind direction, the correlation coefficient is 0.94 with a very small value of 1.3° in mean wind direction bias and an rms deviation of 38° for all wind conditions. When excluding the low wind range of 4–12 knots, the rms deviation in wind direction reduces to 22°. Considering QSCAT requirements designed for ocean wind measurements and actual evaluations of QSCAT performance over ocean, results for high-resolution lake wind vectors indicate that QSCAT performs well over the Great Lakes. Moreover, we show that wind fields derived from satellite scatterometer data before, during, and after a large storm in October 1999, with winds stronger than 50 knots, can monitor the storm development over large scales. The satellite results for storm monitoring are consistent with GLCFS nowcast winds and lake buoy measurements. A geophysical model function can be developed specifically for the Great Lakes using long-term data from satellite scatterometers, to derive more accurate wind fields for operational applications as well as scientific studies.
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