Map showing the bathymetry of the Gulf of Mexico and regional physiographic features. Characterizations of bottom shear stress and sea floor mobility in this database extend offshore to approximately the 120-m isobath. |
Publication Date: June 2014
The Gulf of Mexico region extends from the southeast coast of Texas eastward to the Florida Keys. Very shallow regions around the Mississippi River Delta are not resolved.
Spatially and temporally resolved estimates of bottom shear stress are calculated for seasonal and annual time periods. Seasons are defined as Winter (December-February), Spring (March-May), Summer (June-August), and Fall (September-November).
Specifications for stress and mobility time series:
Datasets used to compute the bottom stress and sediment mobility time series:
Complete details on the procedure used to create the data files may be found in the associated metadata
Suggested citation: Dalyander, P.S., Butman, B., Sherwood, C.R., and Signell, R.P., 2012, U.S. Geological Survey sea floor stress and sediment mobility database: U.S. Geological Survey data release, https://doi.org/10.5066/P999PY84.
Statistics of sea floor wave-current stress and sediment mobility in Arc polygon and point shapefile format for the South Atlantic Bight from model output. Stress statistics are determined for the entire model grid, whereas mobility statistics are determined only at locations where sediment texture data are available. See metadata files for details of the calculations. Click on zip file to download.
Data Layer Name and Explanation |
Preview | Metadata | Download |
---|---|---|---|
Median of Bottom Shear Stress |
GMEX_median.zip | ||
Interpercentile Range of Bottom Shear Stress |
HTML FAQ TEXT XML |
GMEX_hIPR.zip | |
95th Percentile of Bottom Shear Stress |
HTML FAQ TEXT XML |
GMEX_95th_perc.zip | |
Bed Mobility Percentage |
HTML FAQ TEXT XML |
GMEX_mobile_perc.zip | |
Bed Mobility Recurrence Interval |
HTML FAQ TEXT XML |
GMEX_mobile_freq.zip |