RB-02-05
Air Quality in Coastal New England Readme File

Ship:			NOAA research vessel Ronald H. Brown
Cruise Start:		Charleston, SC, July 13, 2002
Cruise End:		Portsmouth, NH, July 26, 2002
Chief Scientist:	Tim Bates
System Operator:	Jonathan Shannahoff
Expocode:               33RO20020713

Method:
Infrared absorption of dried gas.  For details of the system see: 
Measurement of fugacity of Carbon Dioxide in surface water and air using continuous 
sampling methods.  Wanninkhof and Thoning, 1993 in Marine Chemistry 44, 189-205, 
And:
Feely, R.A., R. Wanninkhof, H.B. Milburn, C.E. Cosca, M. Stapp, and P.P. Murphy, 
A new automated underway system for making high precision pCO2 measurements 
onboard research ships, Analytica Chim. Acta, 377, 185-191, 1998.

The three standard gases come from CMDL in Boulder and are directly traceable to 
the WMO scale.

Sampling Cycle:
The system runs on an hourly cycle during which 3 standard gases, 3 air 
samples from the bow tower and 8 surface water samples (from the 
equilibrator head space) are analyzed on the following schedule:

Mins. after hour		Sample
4				Low Standard
8				Mid Standard
12				High Standard
16.5				Water
21				Water
25.5				Water
30				Water
34				Air
38				Air
42				Air
46.5				Water
51				Water
55.5				Water
60				Water

Units:
All xCO2 values are reported in parts per million (ppm) and fCO2 values 
are reported in microatmospheres (uatm) assuming 100 % humidity at the 
equilibrator temperature.

Notes:
1.	Any values outside the range of the standards (293.73, 358.87, & 423.28 ppm) 
should be considered approximate (within 5 ppm).  While individual data points above 
423 or below 293 may not be accurate, the general trends should be indicative of the seawater 
chemistry.
2.  Seawater was turned off from July 15 at 0915 to July 16 at 0015 (GMT) due to dirty
water in New York harbor.  All surface water samples during that period have been removed.
3.  Coastal air transects resulted in air concentration values varying from 350-405 ppm
because of air masses originating from land.
4.  The delta fCO2 values were determined using the highly variable air values.


For questions or comments contact:
Bob Castle
4301 Rickenbacker Causeway
Miami, FL 33149
305-361-4418
castle@aoml.noaa.gov