Datové sady / WATER DEPTH and Other Data from FALSTRIA and Other Platforms From Gulf of Mexico and Others from 19870108 to 19870701 (NODC Accession 8700254)


WATER DEPTH and Other Data from FALSTRIA and Other Platforms From Gulf of Mexico and Others from 19870108 to 19870701 (NODC Accession 8700254)

Vydavatel National Oceanic and Atmospheric Administration, Department of Commerce

Datum vydání před téměř 10 roky

US
beta

Shrnutí

Co poskytovatel nabízí?
ongoing release of a series of related datasets

Databázová licence
Nevztahuje se

Licence na obsah
Creative Commons CCZero

Způsob ověření
ověřený automaticky

Popis

Temperature profile data were collected using XBT and BT casts from the NOAA Ship RESEARCHER and other platforms in the Gulf of Mexico and Northwest Atlantic Ocean from 08 January 1987 to 01 July 1987. Data were collected by the Atlantic Oceanographic and Meteorological Laboratory (AOML) Miami, Florida and other institutions with support from the Equatorial Pacific Ocean Climate Studies (EPOCS) and SubTropical Atlantic Climate Studies (STACS) projects. Data were processed by NODC to the NODC standard Universal Bathythermograph Output (UBT) format. Full format description is available from NODC at www.nodc.noaa.gov/General/NODC-Archive/bt.html. The UBT file format is used for temperature-depth profile data obtained using expendable bathythermograph (XBT) instruments. Standard XBTs can obtain profiles at depths of about 450 or 760 m. With special instruments, measurements can be obtained to 1830 m. Cruise information, position, date, and time are reported for each observation. The data record comprises pairs of temperature-depth values. Unlike the MBT data file, in which temperature values are recorded at uniform 5m intervals, the XBT Data File contains temperature values at non-uniform depths. These depths are at a minimum number of points ("inflection points") required to record the temperature curve to an acceptable degree of accuracy. On output, however, the user may request temperature values either at inflection points or interpolated to uniform depth increments.