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                <gco:CharacterString>Parameter or Variable: Total alkalinity;
Abbreviation: TA;
Unit: Î¼mol/kg;
Observation type: Model output;
In-situ / Manipulation / Response variable: response variable;
Measured or calculated: Calculated;
Detailed sampling and analyzing information: Algorithms are derived to determine the partial pressure of CO2 (pCO2) in surface water for five different regions on the east coast. These algorithms use optimally interpolated sea surface temperature (SST) products that merge multiple satellites, sea surface salinity (SSS) and chlorophyll-a. The algorithms are described in Signorini SR, et al. (2013). The TA-SSS-SST (Total Alkalinity / Sea Surface Salinity / Sea Surface Temperature) relationships are SSS dependent: SSS &lt; 32.45 TA = (42.6 * SSS) + 815.9 SSS &gt;= 32.45 TA = (61.9 * SSS) + 190.0 These linear relationships are based on coastal cruises GOMECC 1 and 2 data and account for non-zero alkalinity from riverine outflows for the low salinity algorithm (Wang et al. 2017). Data Sources 2014-2017: SST http://data.remss.com/SST/daily/mw_ir/v05.0/netcdf/ SSS https://hycom.org/data/glba0pt08/expt-91pt2 Chlâa https://oceandata.sci.gsfc.nasa.gov/MODIS-Aqua/Mapped/Monthly/4km/chlor_a/ Data Sources 2018 to 2020: SST ftp://ftp.remss.com/sst/daily/mw_ir/v05.0/netcdf/ SSS ftp://ftp.remss.com/smap/SSS/V04.0/FINAL/L3/monthly/2019/ Chlâa https://oceandata.sci.gsfc.nasa.gov/VIIRS-SNPP/Mapped/Monthly/4km/chlor_a/ Wang, Z. A., G. L. Lawson, C. H. Pilskaln, and A. E. Maas (2017), Seasonal controls of aragonite saturation states in the Gulf of Maine, J. Geophys. Res. Oceans, 122, https://doi.org/10.1002/2016JC012373.</gco:CharacterString>
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Abbreviation: pH;
Observation type: Model output;
In-situ / Manipulation / Response variable: response variable;
Measured or calculated: Calculated;
Detailed sampling and analyzing information: Algorithms are derived to determine the partial pressure of CO2 (pCO2) in surface water for five different regions on the east coast. These algorithms use optimally interpolated sea surface temperature (SST) products that merge multiple satellites, sea surface salinity (SSS) and chlorophyll-a. The algorithms are described in Signorini SR, et al. (2013). Using the computed pCO2 and TA all other variables were computed using standard CO2SYS algorithms. Signorini, S. R., A. Mannino, R. G. Najjar, Jr., M. A. M. Friedrichs, W.-J. Cai, J. Salisbury, Z. Al-eck Wang, H. Thomas, and E. Shadwick (2013), Surface ocean pCO2 seasonality and sea-air CO2 flux estimates for the North American east coast, J. Geophys. Res. Oceans, 118, 5439-5460, https://doi.org/10.1002/jgrc.20369.</gco:CharacterString>
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Abbreviation: pCO2;
Observation type: Model output;
In-situ / Manipulation / Response variable: response variable;
Measured or calculated: Calculated;
Detailed sampling and analyzing information: Algorithms are derived to determine the partial pressure of CO2 (pCO2) in surface water for five different regions on the east coast. These algorithms use optimally interpolated sea surface temperature (SST) products that merge multiple satellites, sea surface salinity (SSS) and chlorophyll-a. The algorithms are described in Signorini SR, et al. (2013). Data Sources 2014-2017: SST http://data.remss.com/SST/daily/mw_ir/v05.0/netcdf/ SSS https://hycom.org/data/glba0pt08/expt-91pt2 Chlâa https://oceandata.sci.gsfc.nasa.gov/MODIS-Aqua/Mapped/Monthly/4km/chlor_a/ Data Sources 2018 to 2020: SST ftp://ftp.remss.com/sst/daily/mw_ir/v05.0/netcdf/2019/ SSS ftp://ftp.remss.com/smap/SSS/V04.0/FINAL/L3/monthly/2019/ Chlâa https://oceandata.sci.gsfc.nasa.gov/VIIRS-SNPP/Mapped/Monthly/4km/chlor_a/ Signorini, S. R., A. Mannino, R. G. Najjar, Jr., M. A. M. Friedrichs, W.-J. Cai, J. Salisbury, Z. Al-eck Wang, H. Thomas, and E. Shadwick (2013), Surface ocean pCO2 seasonality and sea-air CO2 flux estimates for the North American east coast, J. Geophys. Res. Oceans, 118, 5439-5460, https://doi.org/10.1002/jgrc.20369.</gco:CharacterString>
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                <gco:CharacterString>Parameter or Variable: Aragonite saturation state;
Abbreviation: omegaAr;
Observation type: Model output;
In-situ / Manipulation / Response variable: response variable;
Measured or calculated: Calculated;
Detailed sampling and analyzing information: Algorithms are derived to determine the partial pressure of CO2 (pCO2) in surface water for five different regions on the east coast. These algorithms use optimally interpolated sea surface temperature (SST) products that merge multiple satellites, sea surface salinity (SSS) and chlorophyll-a. The algorithms are described in Signorini SR, et al. (2013). The TA-SSS-SST (Total Alkalinity / Sea Surface Salinity / Sea Surface Temperature) relationships are SSS dependent: SSS &lt; 32.45 TA = (42.6 * SSS) + 815.9 SSS &gt;= 32.45 TA = (61.9 * SSS) + 190.0 These linear relationships are based on coastal cruises GOMECC 1 and 2 data and account for non-zero alkalinity from riverine outflows for the low salinity algorithm (Wang et al. 2017). Using the computed pCO2 and TA all other variables were computed using standard CO2SYS algorithms. Data Sources 2014-2017: SST http://data.remss.com/SST/daily/mw_ir/v05.0/netcdf/ SSS https://hycom.org/data/glba0pt08/expt-91pt2 Chlâa https://oceandata.sci.gsfc.nasa.gov/MODIS-Aqua/Mapped/Monthly/4km/chlor_a/ Data Sources 2018 to 2020: SST ftp://ftp.remss.com/sst/daily/mw_ir/v05.0/netcdf/2019/ SSS ftp://ftp.remss.com/smap/SSS/V04.0/FINAL/L3/monthly/2019/ Chlâa https://oceandata.sci.gsfc.nasa.gov/VIIRS-SNPP/Mapped/Monthly/4km/chlor_a/ Signorini, S. R., A. Mannino, R. G. Najjar, Jr., M. A. M. Friedrichs, W.-J. Cai, J. Salisbury, Z. Al-eck Wang, H. Thomas, and E. Shadwick (2013), Surface ocean pCO2 seasonality and sea-air CO2 flux estimates for the North American east coast, J. Geophys. Res. Oceans, 118, 5439-5460, https://doi.org/10.1002/jgrc.20369. Wang, Z. A., G. L. Lawson, C. H. Pilskaln, and A. E. Maas (2017), Seasonal controls of aragonite saturation states in the Gulf of Maine, J. Geophys. Res. Oceans, 122, https://doi.org/10.1002/2016JC012373.</gco:CharacterString>
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Abbreviation: omegaCa;
Observation type: Model output;
In-situ / Manipulation / Response variable: response variable;
Measured or calculated: Calculated;
Detailed sampling and analyzing information: Algorithms are derived to determine the partial pressure of CO2 (pCO2) in surface water for five different regions on the east coast. These algorithms use optimally interpolated sea surface temperature (SST) products that merge multiple satellites, sea surface salinity (SSS) and chlorophyll-a. The algorithms are described in Signorini SR, et al. (2013). The TA-SSS-SST (Total Alkalinity / Sea Surface Salinity / Sea Surface Temperature) relationships are SSS dependent: SSS &lt; 32.45 TA = (42.6 * SSS) + 815.9 SSS &gt;= 32.45 TA = (61.9 * SSS) + 190.0 These linear relationships are based on coastal cruises GOMECC 1 and 2 data and account for non-zero alkalinity from riverine outflows for the low salinity algorithm (Wang et al. 2017). Using the computed pCO2 and TA all other variables were computed using standard CO2SYS algorithms. Data Sources 2014-2017: SST http://data.remss.com/SST/daily/mw_ir/v05.0/netcdf/ SSS https://hycom.org/data/glba0pt08/expt-91pt2 Chlâa https://oceandata.sci.gsfc.nasa.gov/MODIS-Aqua/Mapped/Monthly/4km/chlor_a/ Data Sources 2018 to 2020: SST ftp://ftp.remss.com/sst/daily/mw_ir/v05.0/netcdf/2019/ SSS ftp://ftp.remss.com/smap/SSS/V04.0/FINAL/L3/monthly/2019/ Chlâa https://oceandata.sci.gsfc.nasa.gov/VIIRS-SNPP/Mapped/Monthly/4km/chlor_a/ Signorini, S. R., A. Mannino, R. G. Najjar, Jr., M. A. M. Friedrichs, W.-J. Cai, J. Salisbury, Z. Al-eck Wang, H. Thomas, and E. Shadwick (2013), Surface ocean pCO2 seasonality and sea-air CO2 flux estimates for the North American east coast, J. Geophys. Res. Oceans, 118, 5439-5460, https://doi.org/10.1002/jgrc.20369. Wang, Z. A., G. L. Lawson, C. H. Pilskaln, and A. E. Maas (2017), Seasonal controls of aragonite saturation states in the Gulf of Maine, J. Geophys. Res. Oceans, 122, https://doi.org/10.1002/2016JC012373.</gco:CharacterString>
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