The Ocean Bottom Properties Database

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The point of this page is to share information on the construction of an Ocean Bottom Properties (OBT) database.  By far, temperature is the most frequently recorded variable at ocean depth - there are many different ways to record temperature (bolltes, CTDs, XBTs, reversing thermometers, etc.).  Second is salinity, measured in bottle collections or via CTD.  The other measured variable in this database are dissolved oxygen, nitrate, nitrite, inorganic phosphate, ph, and  silicate.  The impetus for this work is the complete lack of a database equivalent to the COADS (Comprehensive Ocean Atmosphere Data Set) for the ocean bottom.  I wanted such a database for my work in modeling historical changes in halibut (a demersal groundfish) size at age.  Seems to me that scientists who work with other species of groundfish might also appreciate historical data on oceanographic properties of the water in which these fish reside.

I am NOT contructing a database for the world's oceans, only the Alaskan and West Coast continental shelf.  The database has the following boundary conditions

To date (28 October 1998), I have acquired data from the following sources.  Click to see a gif of the database locations.  Note that these map show all stations from all years, all months.  the trick is to figure out what amount of aggregation is required for a proper analysis.

All data - all kinds, all locations, all times

NODC bottle data from the kind folks out at the National Oceanographic Data Center.  It took a long time to get this data, but it was worth it.

NODC mbt data from the same folks.  MBT = mechanical bathythermograph, an old fashioned way to get temperature at depth

NODC xbt data from the same folks.  XBT = expendable bathythermograph, a new fashioned way to get temperature at depth

NODC ctd data from the same folks.  CTD = conductivity, temperature, depth.  These data are collected by instruments that measure temperature by thermistor, salinity by conductivity, and depth by pressure.

Ocean bottom temperature data from NOAA/NMFS/RACE research surveys

Ocean bottom temperature data from International Pacific Halibut Commission (chez moi!)

Ocean bottom temperature data from Russian bottom trawl surveys
 

Using all the data sources, here are temperature data locations by decade (jpg files)
  1930s | 1940s | 1950s  | 1960s | 1970s | 1980s | 1990s

Here are more detailed plots of data by month from 1950-1997 (ps files)
1950-52 | 1953-55 | 1956-58 | 1959-61 | 1962-64 | 1965-67 | 1968-70 | 1971-73
1974-76 | 1977-79 | 1980-82 | 1983-85 | 1986-88 | 1989-91 | 1992-94 | 1995-97
 
 

Hypotheses and Findings

Did the Bering Sea and Gulf of Alaska bottom waters warm up following the climate regime shift of 1977?  And by how much?  There has been talk of a climate regime shift in 1989, is there evidence of a change in ocean bottom properties?

Many different analyses can be conducted.  Here a few so far.

First, some average temperature plots.
Monthly averages for the 1950-96 period (ps file)
Long-term average for 1950-96, averaged across months May-Sept.
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Now, some multiple plots using differencing to identify temporal changes in bottom temperatures.  The following graphics each have three panels.  The bottom panel show the average bottom temperature for the five year period (averaged across months May-Sept.).  the middle panel shows the change in bottom temperature from the previous pentad (i.e. a difference map where the early pentad tempature at each location is subtracted from the later pentad temperature).  Positive temepratures indicate a warming from one pentad to the next.  The third panel shows the difference between the pentad bottom temperatures and the long term mean (1950-96, May-Oct.).  Positive temperatures indicate pentad temperatures are warmer than the long term mean.
1960-64 | 1965-69 | 1970-74 | 1975-79 | 1980-84 | 1985-89 | 1990-94 | 1995-99
 

To begin to quantify interannual/decadal variability I made some annual areal averages.  Initially, I selected five regions with the coordinates listed below.  For this attempt, I averaged all observation for months May-September within the region to obtain an average for each year.  If there were less than 10 observations for a given year, no average value was computed.  The linked graphics are jpg files.
NW Bering Shelf: lat:60-64, lon: 184-192
SE Bering shelf: lat: 56-58, lon: 186-194
Western Gulf: lat: 56-60, lat: 204-212
Eastern Gulf: lat: 54-60 long: 220-228
British Columbia: lat: 48-54, lon: 228-234
 


If you have comments or suggestions, email me at