The extended records (files with an "ext" qualifier) are comprised of smoothed values, and interpolated and extrapolated values defined at each time step of the synchronization period. Those who wish to use extended records in their modeling application must simply add the reference MBL vector (COLUMN 3) to the difference climatology (COLUMN 4), i.e., extended record = REF + diff. Users will notice that S(t) = REF + diff wherever smoothed values (COLUMN 2) exist.

You may also choose to use only the smoothed values (COLUMN 2) from the sites that are synchronized which will have assigned default values where there are no measurements.

PLEASE NOTE: Occasional discontinuities at the transition between smoothed values and extrapolated values may be significant in certain modeling applications. These occur when values derived from data extension techniques (based on average behavior) join actual measurements that depart from average behavior. Discontinuities may occur at either end of the smoothed measurement record.

PLEASE NOTE: Discontinuities within periods of interpolated or extrapolated values may occur when MBL measurement records begin, end, or are interrupted for long periods of time. Some discontinuities may be significant in certain modeling applications. Serious discontinuities are identified below.

Time step Latitude1 Cause
1984.208333 5°N ESRL sampling program at Christmas Island, Kiribati (CHR) begins
1985.354167 28°N ESRL sampling program at Sand Island, Midway (MID) begins
1987.000000 25°S ESRL shipboard sampling in Pacific Ocean (POC) begins
1989.125000 32°N ESRL sampling program at Bermuda (BME, BMW) begins
1998.187500 43°N ESRL sampling program at Cape Meares, Oregon (CMO) ends
2008.833333 32°N ESRL sampling gap at Bermuda East (BME)
1Specifies the 5° latitude band most strongly influenced by the change in the MBL measurement distribution

PLEASE NOTE: The data extension procedure requires at least 2 years of observations.

Relative weighting of each value in an extended record can be important because some points are better determined than others. Confidence in the smoothed values depends on the density of the data, the relative occurrence of rejected data, the "scatter" in the data, the type and number of corrections applied, and the length of the measurement period. Masarie and Tans [1995] describe in detail the relative weighting scheme and provide an example of how extended records and relative weights have been used in a 2-D modeling application. Users may choose to ignore our weighting scheme; sufficient information is included in the weight files so that users may devise their own weighting scheme.