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The half interpercentile range of bottom shear stress for the Gulf of Maine...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of... -
U.S. Geological Survey calculated half interpercentile range (half of the...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of... -
The half-interpercentile range of bottom shear stress for the Gulf of...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of... -
The half-interpercentile range of bottom shear stress for the Gulf of...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of... -
The half-interpercentile range of bottom shear stress for the Gulf of...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of... -
U.S. Geological Survey calculated half interpercentile range (half of the...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of... -
The half-interpercentile range of bottom shear stress for the Gulf of...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of... -
U.S. Geological Survey calculated half interpercentile range (half of the...
The U.S. Geological Survey has been characterizing the regional variation in shear stress on the sea floor and sediment mobility through statistical descriptors. The purpose of...