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Atmospheric Carbon Monoxide Dry Air Mole Fractions from the
NOAA ESRL GMD Carbon Cycle Surface Network

Version: 2011-03-17
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CONTENTS

1.       Data source and contacts
2.       Use of data
2.1      Citation
3.       Reciprocity 
4.       Warnings
5.       Update notes
6.       Introduction
7.       DATA - General Comments
7.1      DATA - Sampling Locations
7.2      DATA - File Name Description
7.3      DATA - Event
7.4      DATA - QC Flags
8.       Data retrieval
9.       References

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1. DATA SOURCE AND CONTACTS

National Oceanic and Atmospheric Administration (NOAA)
Earth System Research Laboratory (ESRL)
Global Monitoring Division (GMD)
Carbon Cycle Greenhouse Gases (CCGG)

Correspondence concerning these data should be directed to:

Paul Novelli and Arlyn Andrews
NOAA ESRL Global Monitoring Division
325 Broadway, GMD-1
Boulder, CO  80305
U.S.A.

email:    Arlyn.Andrews@noaa.gov
          Paul.C.Novelli@noaa.gov


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2. USE OF DATA

These data are made freely available to the public and the
scientific community in the belief that their wide dissemination
will lead to greater understanding and new scientific insights.
The availability of these data does not constitute publication
of the data.  NOAA relies on the ethics and integrity of the user to
assure that ESRL receives fair credit for their work.  If the data 
are obtained for potential use in a publication or presentation, 
ESRL should be informed at the outset of the nature of this work.  
If the ESRL data are essential to the work, or if an important 
result or conclusion depends on the ESRL data, co-authorship
may be appropriate.  This should be discussed at an early stage in
the work.  Manuscripts using the ESRL data should be sent to ESRL
for review before they are submitted for publication so we can
insure that the quality and limitations of the data are accurately
represented.

2.1 CITATION

Please reference these data as

   A. E. Andrews  and P. C. Novelli (2010), Carbon
   Monoxide Dry Air Mole Fractions from the NOAA ESRL 
   Surface Network using Programmable Flask Packages
   (PFP), 2006-2010, Version: 2011-03-17.


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3. RECIPROCITY

Use of these data implies an agreement to reciprocate.
Laboratories making similar measurements agree to make their
own data available to the general public and to the scientific
community in an equally complete and easily accessible form.
Modelers are encouraged to make available to the community,
upon request, their own tools used in the interpretation
of the ESRL data, namely well documented model code, transport
fields, and additional information necessary for other
scientists to repeat the work and to run modified versions.
Model availability includes collaborative support for new
users of the models.

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4. WARNINGS

Every effort is made to produce the most accurate and precise
measurements possible.  However, we reserve the right to make
corrections to the data based on recalibration of standard gases
or for other reasons deemed scientifically justified.

We are not responsible for results and conclusions based on use
of these data without regard to this warning.


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5. UPDATE NOTES


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6. INTRODUCTION

A "Programmable Flask Package" was developed in the early 1990s for
use in our aircraft project to collect vertical profiles of air
samples.  These packages (PFPs) are analyzed on the same analytical
systems used for the CCGG's global cooperative air sampling network
samples to measure CO2, CH4, CO, H2, N2O, and SF6.  Many of the PFPs
are also analzed by the HATS group by GCMS for a suite of CFCs, HFCs,
HCFCs, NMHCs, and a few other species.

As a quality control step, we began deploying PFPs at some surface
sites in 2006.  Most of these sites are tall towers, where the PFP
measurements can be compared with continuous in situ measurements of
CO2 and CO.  Samples are collected approximately daily from one of 
the tower intakes.

Measurements from NOAA ESRL Carbon Cycle Vertical 
Profile Network are reported in units of nanomol/mol
(10^-9 mol CO per mol of dry air (nmol/mol) or parts 
per billion (ppb)).


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7. DATA - GENERAL COMMENTS

Ambient and standard air samples are injected into the gas
chromatograph (GC). Carbon monoxide (CO) and molecular hydrogen
(H2) are separated from other sample constituents using dual
columns. CO and H2 are reacted with hot HgO bed to produce
mercury (Hg).  Hg is then determined photometrically. The method
can be non linear. Since 2007 we have also used a CO detector 
based on resonance fluorescence in the VUV. This method is linear
over the range of the remote atmosphere.

The non-linear HgO detector requires a multipoint calibration
(we use 6 standards in the atmospheric range). This process
is highly automated for field and laboratory operations.
Measurements are reported in units of nanomol/mol (10^-9 mol
CO per mol of dry air (nmol/mol) or parts per billion (ppb))
relative to the WMO CO scale (Novelli et al., 1991, Novelli
et al., 1994, Novelli et al., 1998).  Reproducibility of our
measurements, based on repeated analysis of air from a
high-pressure cylinder, is 1 nmol/mol at 50 nmol/mol and
2 nmol/mol at 200 nmol/mol over the period of our
measurements. The absolute accuracy of our CO scale is
unknown.


Calibration of the GC covers the range of the marine background 
troposphere (~ 50 and 200 ppb).  Mixing ratios above and below 
the calibrated span contain greater uncertainty relative to 
those within the calibration.  Estimated errors relative to the 
calibrated span for between 35-50ppb and 200-230ppb are less 
than +/- 1-2%, however mixing ratios below 25 ppb and above 
230 ppb should be used with caution as errors can be
substantially larger and therefore may not be suitable for 
quantitative analysis.  CO results considered out of range are 
flagged with a "C" in the 3rd column (see Section 7.4 DATA 
- QC Flags). Calibration of the VUV instrument uses a single
reference gas of ~125 ppb. 

Sampling frequencies are approximately daily.

The air samples are collected using an automated Programmable Flask
Package (PFP).

7.1 DATA - SAMPLING LOCATIONS

Table of NOAA GMD aircraft sampling sites.


The table includes the three letter code used to identify each
site; the site name; latitude, longitude, and altitude (meters
above sea level) of the sampling location; the first and last sample 
dates; and sampling status.

Note: Data for all species may not be available for all sites listed 
in the table.

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7.2 DATA - FILE NAME DESCRIPTION

Encoded into each file name are the sampling location, platform, and
strategy; measurement laboratory; file content; and gas identifier.
All file names use the following naming scheme:

 1     2               3     4         5          6           7
[site][data grouping]_[lab#][strategy][platform]_[qualifier].[gas]

1. [Sampling site]
   (ex) brw_, poc_, car_, amt_

2. [Grouping of data within the file]

   Data may be grouped by date, latitude, longitude, altitude, etc.
   
   If data are grouped by date then identifier has yyyy[mm][dd] format.
   (ex) brw2005_, amt200403_, lef20050315_

   If the sampling platform is an aircraft then the identifier is a
   3-character numeric field with units of 10^2 meters (hm) above sea level.
   (ex) car040_, haa005_

   If the sampling platform is a ship then the identifier is a 3-character 
   alphanumeric field with units of degrees (00-90).  Bins in the northern 
   and southern hemispheres are denoted as n## and s## respectively.  The 
   equatorial bin is denoted as 000.
   (ex) pocs25_, poc000_, scsn03_

3. [Measurement laboratory]

   A two character numeric field identifies the measurement laboratory (01-99).
   NOAA ESRL is lab number 01 (see https://om.cmdl.noaa.gov/globalview/labs/).

4. [Sampling strategy]

   A single alphanumeric character (0-9,a-z,A-Z) indicates the sampling strategy.

   _??C               Semi-continuous
   _??D               Discrete using Portable Sampling Unit (PSU)
   _??P               Discrete using Programmable Flask Package (PFP)

5. [Sampling platform]

   A single alphanumeric character (0-9,a-z,A-Z) indicates the sampling platform.

   _???0              Land
   _???1              Ship
   _???2              Aircraft
   _???3              Tower

6. [Qualifier]

   An alphanumeric string describes the type of data included in the file.

   _????_event        Data from every collection event
   _????_mm           Computed monthly mean values
   _????_hr           Computed hourly averages (semi-continuous data only)
   _????_day          Computed daily averages (semi-continuous data only)
   _????_all          All Data

7. [Gas]

   Identifies the trace gas species.

   _????_???.co2      Carbon dioxide
   _????_???.ch4      Methane
   _????_???.co2c13   d13C (co2)

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7.3 DATA - EVENT

The data files in "ccg/co/event/" use the following naming
scheme (see Section 7.2):

     xxx_01P0_event.co

(ex) lef_01P0_event.co contains LEF co surface data

The data files contain multiple lines of header information
followed by one line for each atmospheric measurement.

Fields are defined as follows:

Field 1:    [SITE CODE] The three-character sampling location code (see above).

Field 2:    [YEAR] The sample collection date and time in UTC.
Field 3:    [MONTH]
Field 4:    [DAY]
Field 5:    [HOUR]
Field 6:    [MINUTE]

Field 7:    [FLASK ID] The sample container ID.

Field 8:    [METHOD] A single-character code that identifies the sample 
             collection method.  The codes are:

             A - Sample collected using a Programmable Flask Package (PFP).

Field 9:    [TRACE GAS NAME] Gas identifier (e.g., co2, co2c13).

Field 10:   [MEASURED VALUE] Dry air mole fraction or isotopic composition.  
             Missing values are denoted by -999.99[9].

Field 11:   [ESTIMATED UNCERTAINTY] Estimated uncertainty of the reported
             measurement value.  Missing values are denoted by -999.99[9].

Field 12:   [QC FLAG] A three-character field indicating the results of our
             data rejection and selection process, described in section 7.4.

Field 13:   [INSTRUMENT] A 2-character code that identifies the instrument
             used for the measurement.

Field 14:   [YEAR] The measurement date and time in LT.
Field 15:   [MONTH]
Field 16:   [DAY]
Field 17:   [HOUR]
Field 18:   [MINUTE]

Field 19:   [LATITUDE] The latitude where the sample was collected, (negative (-)
             numbers indicate samples collected in the southern hemipshere).

Field 20:   [LONGITUDE] The longitude where the sample was collected, (negative (-)
             numbers indicate samples collected in the western hemisphere).

Field 21:   [ALTITUDE] The altitude where the sample was collected (masl).

Field 22:   [EVENT NUMBER] A long integer that uniquely identifies the sampling
             event.

Fields in each line are delimited by whitespace.

(ex)

WKT 2010 08 10 20 31 3083-12 A co2 387.940 -999.990 ..P L8 2010 08 19 03 07  31.3200  -97.3300   708.05   302117

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7.4 QC FLAGS

NOAA ESRL uses a 3-column quality control flag where each column
is defined as follows:

column 1    REJECTION flag.  An alphanumeric other
            than a period (.) in the FIRST column indicates
            a sample with obvious problems during collection
            or analysis.  This measurement should not be interpreted.

column 2    SELECTION flag.  An alphanumeric other than a
            period (.) in the SECOND column indicates a sample
            that is likely valid but does not meet selection
            criteria determined by the goals of a particular
            investigation.

column 3    COMMENT flag.  An alphanumeric other than a period (.) 
            in the THIRD column provides additional information 
            about the collection or analysis of the sample.

            WARNING: A "P" in the 3rd column of the QC flag indicates
            the measurement result is preliminary and has not yet been 
            carefully examined by the PI.  The "P" flag is removed once 
            the quality of the measurement has been determined.

If both the first and second column contain a period (e.g., "..." and "..I"),
the sample is RETAINED.


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8. DATA RETRIEVAL

To transfer all files in a directory, it is more efficient to 
download the tar or zipped files.  

To transfer a tar file, use the following steps from the ftp prompt:

   1. ftp> binary                    ! set transfer mode to binary
   2. ftp> get filename.tar.gz       ! transfer the file
   3. ftp> bye                       ! leave ftp

   4. $ gunzip filename.tar.gz       ! unzip your local copy
   5. $ tar xvf filename.tar         ! unpack the file

To transfer a zipped file, use the following steps from the ftp prompt:

   1. ftp> binary                    ! set transfer mode to binary
   2. ftp> get filename.zip          ! transfer the file
   3. ftp> bye                       ! leave ftp

   4. $ unzip filename.zip           ! uncompress your local copy

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9. REFERENCES

Lang, P.M., L.P. Steele, R.C. Martin, and K.A. Masarie,
  Atmospheric methane data for the period 1983-1985 from
  the NOAA/GMCC global cooperative flask sampling network,
  NOAA Technical Memorandum ERL CMDL-1, 1990a.

Lang, P.M., L.P. Steele, and R.C. Martin, Atmospheric
  methane data for the period 1986-1988 from the NOAA/CMDL
  global cooperative flask sampling network, NOAA Technical
  Memorandum ERL CMDL-2, 1990b.

Novelli, P.C., J.E. Elkins, and L.P. Steele, The development
  and evaluation of a gravimetric reference scale for
  measurements of atmospheric carbon monoxide, J. Geophys.
  Res., 96, 13,109-13,121, 1991.

Novelli, P.C., L.P. Steele, and P.P. Tans, Mixing ratios of
  carbon monoxide in the troposphere, J. Geophys. Res., 97,
  20,731-20,750, 1992.

Novelli, P.C., J.E. Collins, Jr, R.C. Myers, G.W. Sachse,
  and H.E. Scheel, Reevaluation of the NOAA/CMDL carbon
  monoxide reference scale and comparisons to CO reference
  gases at NASA-Langley and the Fraunhofer Institute, 99,
  12,833- 12,839, 1994.

Novelli, P.C., K.A. Masarie, and P.M. Lang, Distributions
  and recent changes in carbon monoxide in the lower
  troposphere, J. Geophys. Res., 103, 19,1015- 19,033, 1998.

Novelli, P.C., K.A. Masarie, P.M. Lang, B.D. Hall, R.C. Myers,
  and J.W. Elkins, Re-analysis of tropospheric CO trends:
  Effects of the 1997-1998 wild fires, J. Geophys. Res., 108,
  D15 : 4464, doi:10.1029/2002JD003031, 2003.

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