cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.899342
title: Quantitative reconstruction of Holocene sea ice and sea surface temperature off West Greenland from the first regional diatom dataset (transfer function)

description: Holocene oceanographic conditions in Disko Bay, West Greenland were reconstructed from high-resolution diatom records derived from two marine sediment cores. A modern dataset composed of 35 dated surface sediment samples collected along the entire West Greenland coast accompanied by remote sensing data were used to develop a diatom transfer function to reconstruct April Sea Ice Concentration (SIC) supported by July Sea Surface Temperature (SST) in the area. Our quantitative reconstruction shows that oceanographic changes recorded throughout the last c. 11000 years reflect seasonal interplay between spring (April SIC) and summer (July SST) conditions. Our records show clear correlation with climate patterns identified from ice core data from GISP2 and Agassiz-Renland for the early to mid Holocene. The early Holocene deglaciation of western Greenland Ice Sheet was characterised in Disko Bay by initial strong centennial-scale fluctuations in April SIC with amplitude of over 40%, followed by high April SIC and July SST. These conditions correspond to a general warming of the climate in the Northern Hemisphere. A decrease in April SIC and July SST was recorded during the Holocene Thermal Optimum reflecting more stable spring-summer conditions in Disko Bay. During the late Holocene, high April SIC characterised the Medieval Climate Anomaly, while high July SST prevailed during the Little Ice Age, supporting previously identified anti-phase relationship between surface waters in West Greenland and climate in NW Europe. This anti-phase pattern might reflect seasonal variations in regional oceanographic conditions and large-scale fluctuations within the North Atlantic Oscillation and Atlantic Meridional Overturning Circulation.
description: Supplement to: Krawczyk, Diana Wioletta; Witkowski, A; Moros, Matthias; Lloyd, Jeremy M; Høyer, J L; Miettinen, Arto; Kuijpers, Antoon (2017): Quantitative reconstruction of Holocene sea ice and sea surface temperature off West Greenland from the first regional diatom data set. Paleoceanography, 32(1), 18-40
DOI: 10.1594/pangaea.900271
title: Alkenones in sediment core MSM343300
DOI: 10.25549/uschist-ouc18869791
title: Daily Trojan, vol. 39, no. 69, Jan 6, 1948

description: Southern California Daily Trojan, vol. 39, no. 69, January 6, 1948.
DOI: 10.15468/dl.cc7syb
title: Occurrence Download

description: A dataset containing 17736 species occurrences available in GBIF matching the query:
{
 "and" : [
 "TaxonKey is Dacnis flaviventer",
 "Year is greater than or equal to 2000",
 "Year is less than or equal to 2026",
 "HasCoordinate is true"
 ]
}

 The dataset includes 17736 records from 19 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0033422-260208012135463/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.25549/uschist-ouc18870443
title: Daily Trojan, vol. 39, no. 72, Jan 9, 1948

description: Southern California Daily Trojan, vol. 39, no. 72, January 9, 1948.
DOI: 10.25549/uschist-ouc18871165
title: Daily Trojan, vol. 39, no. 75, Feb 10, 1948

description: Southern California Daily Trojan, vol. 39, no. 75, February 10, 1948.
DOI: 10.25549/uschist-ouc18872838
title: Daily Trojan, vol. 39, no. 86, Feb 25, 1948

description: Southern California Daily Trojan, vol. 39, no. 86, February 25, 1948.
DOI: 10.25549/uschist-ouc18875291
title: Daily Trojan, vol. 39, no. 102, Mar 18, 1948

description: Southern California Daily Trojan, vol. 39, no. 102, March 18, 1948.
DOI: 10.25549/uschist-ouc18915864
title: Daily Trojan, vol. 39, no. 110, Apr 2, 1948

description: Southern California Daily Trojan, vol. 39, no. 110, April 2, 1948. This exemplar lacks page 6.
DOI: 10.25549/uschist-ouc18952609
title: Daily Trojan, vol. 39, no. 115, Apr 9, 1948

description: Southern California Daily Trojan, vol. 39, no. 115, April 9, 1948.
DOI: 10.25549/uschist-ouc110731774
title: Daily Trojan, vol. 40, no. 136, May 10, 1949

description: Southern California Daily Trojan, vol. 40, no. 136, May 10, 1949.
DOI: 10.25549/uschist-ouc110731761
title: Daily Trojan, vol. 40, no. 137, May 11, 1949

description: Southern California Daily Trojan, vol. 40, no. 137, May 11, 1949.
DOI: 10.25549/uschist-ouc110731923
title: Daily Trojan, vol. 40, no. 141, May 17, 1949

description: Southern California Daily Trojan, vol. 40, no. 141, May 17, 1949.
DOI: 10.25549/uschist-ouc110731820
title: Daily Trojan, vol. 40, no. 144, May 20, 1949

description: Southern California Daily Trojan, vol. 40, no. 144, May 20, 1949.
DOI: 10.25549/uschist-ouc110731972
title: Summer News, vol. 4, no. 19, Aug 15, 1949

description: Southern California Summer News, vol. 4, no. 19, August 15, 1949.
DOI: 10.25549/uschist-ouc19554189
title: Daily Trojan, vol. 40, no. 43, Nov 11, 1948

description: Southern California Daily Trojan, vol. 40, no. 43, November 11, 1948.
DOI: 10.25549/uschist-ouc19661675
title: Daily Trojan, vol. 40, no. 58, Dec 6, 1948

description: Southern California Daily Trojan, vol. 40, no. 58, December 6, 1948.
DOI: 10.25574/cdc.412
title: Chandra X-ray Observatory Chandra Data Collection for request #412

description: Chandra Data Collection for request #412
description: DOI updated to include the publication's DOI on 2026-02-20-22:30:00
DOI: 10.25549/uschist-ouc19664751
title: Daily Trojan, vol. 40, no. 67, Dec 17, 1948

description: Southern California Daily Trojan, vol. 40, no. 67, December 17, 1948.
DOI: 10.25549/uschist-ouc110731080
title: Daily Trojan, vol. 40, no. 73, Feb 7, 1949

description: Southern California Daily Trojan, vol. 40, no. 73, February 7, 1949.
DOI: 10.25549/uschist-ouc110731097
title: Daily Trojan, vol. 40, no. 76, Feb 10, 1949

description: Southern California Daily Trojan, vol. 40, no. 76, February 10, 1949.
DOI: 10.25549/uschist-ouc110732383
title: Daily Trojan, vol. 41, no. 9, Sep 21, 1949

description: Southern California Daily Trojan, vol. 41, no. 9, September 21, 1949.
DOI: 10.1594/pangaea.897955
title: δ13C values of methane and acetate at time of harvest, and δ13C and δD values of lipids produced by M. barkeri during growth on labeled substrates (ca 0.5%) and deuterated water (D2O, 1%)

description: This dataset has been carefully reviewed and curated in accordance with PANGAEA's exceptionally high quality standards. However, due to discontinued communication from the authors' side, it did not receive the usual formal approval by the authors and therefore lacks final scientific validation.
DOI: 10.25549/uschist-ouc110732433
title: Daily Trojan, vol. 41, no. 16, Sep 30, 1949

description: Southern California Daily Trojan, vol. 41, no. 16, September 30, 1949.
DOI: 10.1594/pangaea.906043
title: Monthly geometric annual cycle of BrO vertical column densities per instrument

description: Annual Cycle of Geometric BrO VCDs per instrument (for every instrument we averaged the available corresponding months).Projected Area: 70 to 85 Latitude North, -180 to 180 Longitude, Time periods of averaging: GOME (01/03/1996 to 30/06/03), SCIAMACHY (01/09/02 to 31/03/12), GOME-2A (01/03/07 to 30/09/17), GOME-2B (01/03/13 to 30/09/17).
DOI: 10.1594/pangaea.906045
title: Monthly tropospheric annual cycle of BrO vertical column densities per instrument

description: Description: Annual Cycle of Tropospheric BrO VCDs per instrument (for every instrument we averaged the available corresponding months).Projected Area: 70 to 85 Latitude North, -180 to 180 Longitude, Time periods of averaging: GOME (01/03/1996 to 30/06/03), SCIAMACHY (01/09/02 to 31/03/12), GOME-2A (01/03/07 to 30/09/17), GOME-2B (01/03/13 to 30/09/17).
DOI: 10.1594/pangaea.921832
title: Measurements of lipids on submicron aerosol particles at the Cape Verde Islands

description: To investigate the source of lipids and their representatives in the marine atmosphere, concerted measurements of seawater and submicron aerosol particles samples were carried out on the Cape Verde islands. This field study describes the biogenic sources of lipids, their selective transfer from the ocean into the atmosphere and their enrichment as part of organic matter.
DOI: 10.1594/pangaea.921840
title: Measurements of lipids in seawater and on submicron aerosol particles at the Cape Verde Islands: biogenic sources, selective transfer and high enrichments

description: To investigate the source of lipids and their representatives in the marine atmosphere, concerted measurements of seawater and submicron aerosol particles samples were carried out on the Cape Verde islands. This field study describes the biogenic sources of lipids, their selective transfer from the ocean into the atmosphere and their enrichment as part of organic matter.
DOI: 10.15468/dl.2es6fd
title: Occurrence Download

description: A dataset containing 25275972 records in GBIF matching the query:
SELECT
 kingdom,
 kingdomkey,
 phylum,
 phylumkey,
 class,
 classkey,
 "order",
 orderkey,
 family,
 familykey,
 genus,
 genuskey,
 species,
 specieskey,
 "year",
 IF(ISNULL(kingdomkey), NULL, SUM(COUNT(*)) OVER (
 PARTITION BY kingdomkey, "year")) kingdomcount,
 IF(ISNULL(phylumkey), NULL, SUM(COUNT(*)) OVER (
 PARTITION BY phylumkey, "year")) phylumcount,
 IF(ISNULL(classkey), NULL, SUM(COUNT(*)) OVER (
 PARTITION BY classkey, "year")) classcount,
 IF(ISNULL(orderkey), NULL, SUM(COUNT(*)) OVER (
 PARTITION BY orderkey, "year")) ordercount,
 IF(ISNULL(familykey), NULL, SUM(COUNT(*)) OVER (
 PARTITION BY familykey, "year")) familycount,
 IF(ISNULL(genuskey), NULL, SUM(COUNT(*)) OVER (
 PARTITION BY genuskey, "year")) genuscount,
 COUNT(*) occurrences,
 MIN(GBIF_TEMPORALUNCERTAINTY(eventdate, eventtime)) mintemporaluncertainty,
 MIN(COALESCE(coordinateuncertaintyinmeters, 1000)) mincoordinateuncertaintyinmeters
FROM
 occurrence
WHERE
 occurrence.hasgeospatialissues = FALSE
 AND NOT GBIF_STRINGARRAYCONTAINS(occurrence.issue, 'TAXON_MATCH_FUZZY', TRUE)
 AND (occurrence.distancefromcentroidinmeters &gt;= 2000.0 OR occurrence.distancefromcentroidinmeters IS NULL)
 AND NOT occurrence.basisofrecord IN ('FOSSIL_SPECIMEN', 'LIVING_SPECIMEN')
 AND occurrence.occurrencestatus = 'PRESENT'
 AND (occurrence.classificationdetails['d7dddbf4-2cf0-4f39-9b2a-bb099caae36c']['specieskey'] &lt;&gt; '' AND occurrence."year" IS NOT NULL)
GROUP BY
 occurrence.kingdom,
 occurrence.kingdomkey,
 occurrence.phylum,
 occurrence.phylumkey,
 occurrence.class,
 occurrence.classkey,
 occurrence."order",
 occurrence.orderkey,
 occurrence.family,
 occurrence.familykey,
 occurrence.genus,
 occurrence.genuskey,
 occurrence.species,
 occurrence.specieskey,
 occurrence."year"

 The dataset's 25275972 records were derived from 71362 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0033406-260208012135463/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.1594/pangaea.927994
title: M/S Silja Serenade (Helsinki-Stockholm) pCO2 underway measurements in 2018-05

description: Quality control:Measurements during calibration, cleaning, maintenance and low discharge have been removed.-----Flag system:A flag system is applied to the data. Good data that passes the flag control, gets the flag of 11111111. If the raw CO2 partial pressure (not calibration corrected) is out of boundaries (20-1200 ppm), the first digit changes to 9, i.e. if this is only abnormality, the flag would be 9111111. All flags and their boundary limits are listed in the table below.--Flag =&gt; Parameter =&gt; Lower boundary to Upper boundary91111111 =&gt; CO2_ppm_wet =&gt; 20 ppm to 2000 ppm19111111 =&gt; T equ =&gt; -1 °C to 30 °C11911111 =&gt; T tech =&gt; -1 °C to 30 °C11191111 =&gt; Salinity =&gt; 5 to 811119111 =&gt; Pressure =&gt; 0.9 to 1.111111911 =&gt; coeff_A/coeff_B/coeff_C =&gt; -50/0.9/-0.0001 to 100/1.3/0.000111111191 =&gt; SHEQ_flow_LPM/LICOR_flow =&gt; 1.0/50 to N/A/N/A11111119 =&gt; Visually inspected bad data-----Calculations:The CO2 molar fraction observed by the LI-840A is denoted as wet CO2 molar fraction (CO2_ppm_wet).--The molar fraction with respect to dry air is calculated as,CO2_ppm_dry = CO2_ppm_wet / (1 - H2O_ppt/1000),where H2O_ppt is the H2O molar fraction measured by the LI-840A.--For each calibration sequence every 4 hour, a 2nd order polynomial function is fitted to the observed and real molar fractions:CO2_ppm_dry_cal_cor = coeff_A + coeff_B * CO2_ppm_dry + coeff_C * (CO2_ppm_dry)^2Polynomial coefficients (coeff_A, coeff_B and coeff_C) are interpolated between the calibrations.--CO2 partial pressure in dry air is calculated as,pCO2_uatm_dry = CO2_ppm_dry_cal_cor * P_eq_atm--The CO2 partial pressure in wet air (Dickson and Goyet, 1994),pCO2_uatm = pCO2_uatm_dry * (1 - Pws_eq_atm)where saturation water vapor pressure, Pws_eq_atm, is calculated from equilibratortemperature, T_eq_degC (Wagner and PruB, 2002, Eq. 2.5).--Temperature corrected CO2 partial pressure is given for the inlet,pCO2_uatm_temp_corr = pCO2_uatm * exp [ A* (T_in_degC - T_eq_degC)]where A = 0.0423 (Takahashi et al., 1993).
DOI: 10.1594/pangaea.927995
title: M/S Silja Serenade (Helsinki-Stockholm) pCO2 underway measurements in 2018-06

description: Quality control:Measurements during calibration, cleaning, maintenance and low discharge have been removed.-----Flag system:A flag system is applied to the data. Good data that passes the flag control, gets the flag of 11111111. If the raw CO2 partial pressure (not calibration corrected) is out of boundaries (20-1200 ppm), the first digit changes to 9, i.e. if this is only abnormality, the flag would be 9111111. All flags and their boundary limits are listed in the table below.--Flag =&gt; Parameter =&gt; Lower boundary to Upper boundary91111111 =&gt; CO2_ppm_wet =&gt; 20 ppm to 2000 ppm19111111 =&gt; T equ =&gt; -1 °C to 30 °C11911111 =&gt; T tech =&gt; -1 °C to 30 °C11191111 =&gt; Salinity =&gt; 5 to 811119111 =&gt; Pressure =&gt; 0.9 to 1.111111911 =&gt; coeff_A/coeff_B/coeff_C =&gt; -50/0.9/-0.0001 to 100/1.3/0.000111111191 =&gt; SHEQ_flow_LPM/LICOR_flow =&gt; 1.0/50 to N/A/N/A11111119 =&gt; Visually inspected bad data-----Calculations:The CO2 molar fraction observed by the LI-840A is denoted as wet CO2 molar fraction (CO2_ppm_wet).--The molar fraction with respect to dry air is calculated as,CO2_ppm_dry = CO2_ppm_wet / (1 - H2O_ppt/1000),where H2O_ppt is the H2O molar fraction measured by the LI-840A.--For each calibration sequence every 4 hour, a 2nd order polynomial function is fitted to the observed and real molar fractions:CO2_ppm_dry_cal_cor = coeff_A + coeff_B * CO2_ppm_dry + coeff_C * (CO2_ppm_dry)^2Polynomial coefficients (coeff_A, coeff_B and coeff_C) are interpolated between the calibrations.--CO2 partial pressure in dry air is calculated as,pCO2_uatm_dry = CO2_ppm_dry_cal_cor * P_eq_atm--The CO2 partial pressure in wet air (Dickson and Goyet, 1994),pCO2_uatm = pCO2_uatm_dry * (1 - Pws_eq_atm)where saturation water vapor pressure, Pws_eq_atm, is calculated from equilibratortemperature, T_eq_degC (Wagner and PruB, 2002, Eq. 2.5).--Temperature corrected CO2 partial pressure is given for the inlet,pCO2_uatm_temp_corr = pCO2_uatm * exp [ A* (T_in_degC - T_eq_degC)]where A = 0.0423 (Takahashi et al., 1993).
DOI: 10.25549/uschist-ouc110732476
title: Daily Trojan, vol. 41, no. 18, Oct 4, 1949

description: Southern California Daily Trojan, vol. 41, no. 18, October 4, 1949.
DOI: 10.1594/pangaea.927997
title: M/S Silja Serenade (Helsinki-Stockholm) pCO2 underway measurements in 2018-07

description: Quality control:Measurements during calibration, cleaning, maintenance and low discharge have been removed.-----Flag system:A flag system is applied to the data. Good data that passes the flag control, gets the flag of 11111111. If the raw CO2 partial pressure (not calibration corrected) is out of boundaries (20-1200 ppm), the first digit changes to 9, i.e. if this is only abnormality, the flag would be 9111111. All flags and their boundary limits are listed in the table below.--Flag =&gt; Parameter =&gt; Lower boundary to Upper boundary91111111 =&gt; CO2_ppm_wet =&gt; 20 ppm to 2000 ppm19111111 =&gt; T equ =&gt; -1 °C to 30 °C11911111 =&gt; T tech =&gt; -1 °C to 30 °C11191111 =&gt; Salinity =&gt; 5 to 811119111 =&gt; Pressure =&gt; 0.9 to 1.111111911 =&gt; coeff_A/coeff_B/coeff_C =&gt; -50/0.9/-0.0001 to 100/1.3/0.000111111191 =&gt; SHEQ_flow_LPM/LICOR_flow =&gt; 1.0/50 to N/A/N/A11111119 =&gt; Visually inspected bad data-----Calculations:The CO2 molar fraction observed by the LI-840A is denoted as wet CO2 molar fraction (CO2_ppm_wet).--The molar fraction with respect to dry air is calculated as,CO2_ppm_dry = CO2_ppm_wet / (1 - H2O_ppt/1000),where H2O_ppt is the H2O molar fraction measured by the LI-840A.--For each calibration sequence every 4 hour, a 2nd order polynomial function is fitted to the observed and real molar fractions:CO2_ppm_dry_cal_cor = coeff_A + coeff_B * CO2_ppm_dry + coeff_C * (CO2_ppm_dry)^2Polynomial coefficients (coeff_A, coeff_B and coeff_C) are interpolated between the calibrations.--CO2 partial pressure in dry air is calculated as,pCO2_uatm_dry = CO2_ppm_dry_cal_cor * P_eq_atm--The CO2 partial pressure in wet air (Dickson and Goyet, 1994),pCO2_uatm = pCO2_uatm_dry * (1 - Pws_eq_atm)where saturation water vapor pressure, Pws_eq_atm, is calculated from equilibratortemperature, T_eq_degC (Wagner and PruB, 2002, Eq. 2.5).--Temperature corrected CO2 partial pressure is given for the inlet,pCO2_uatm_temp_corr = pCO2_uatm * exp [ A* (T_in_degC - T_eq_degC)]where A = 0.0423 (Takahashi et al., 1993).
DOI: 10.1594/pangaea.927998
title: M/S Silja Serenade (Helsinki-Stockholm) pCO2 underway measurements in 2018-08

description: Quality control:Measurements during calibration, cleaning, maintenance and low discharge have been removed.-----Flag system:A flag system is applied to the data. Good data that passes the flag control, gets the flag of 11111111. If the raw CO2 partial pressure (not calibration corrected) is out of boundaries (20-1200 ppm), the first digit changes to 9, i.e. if this is only abnormality, the flag would be 9111111. All flags and their boundary limits are listed in the table below.--Flag =&gt; Parameter =&gt; Lower boundary to Upper boundary91111111 =&gt; CO2_ppm_wet =&gt; 20 ppm to 2000 ppm19111111 =&gt; T equ =&gt; -1 °C to 30 °C11911111 =&gt; T tech =&gt; -1 °C to 30 °C11191111 =&gt; Salinity =&gt; 5 to 811119111 =&gt; Pressure =&gt; 0.9 to 1.111111911 =&gt; coeff_A/coeff_B/coeff_C =&gt; -50/0.9/-0.0001 to 100/1.3/0.000111111191 =&gt; SHEQ_flow_LPM/LICOR_flow =&gt; 1.0/50 to N/A/N/A11111119 =&gt; Visually inspected bad data-----Calculations:The CO2 molar fraction observed by the LI-840A is denoted as wet CO2 molar fraction (CO2_ppm_wet).--The molar fraction with respect to dry air is calculated as,CO2_ppm_dry = CO2_ppm_wet / (1 - H2O_ppt/1000),where H2O_ppt is the H2O molar fraction measured by the LI-840A.--For each calibration sequence every 4 hour, a 2nd order polynomial function is fitted to the observed and real molar fractions:CO2_ppm_dry_cal_cor = coeff_A + coeff_B * CO2_ppm_dry + coeff_C * (CO2_ppm_dry)^2Polynomial coefficients (coeff_A, coeff_B and coeff_C) are interpolated between the calibrations.--CO2 partial pressure in dry air is calculated as,pCO2_uatm_dry = CO2_ppm_dry_cal_cor * P_eq_atm--The CO2 partial pressure in wet air (Dickson and Goyet, 1994),pCO2_uatm = pCO2_uatm_dry * (1 - Pws_eq_atm)where saturation water vapor pressure, Pws_eq_atm, is calculated from equilibratortemperature, T_eq_degC (Wagner and PruB, 2002, Eq. 2.5).--Temperature corrected CO2 partial pressure is given for the inlet,pCO2_uatm_temp_corr = pCO2_uatm * exp [ A* (T_in_degC - T_eq_degC)]where A = 0.0423 (Takahashi et al., 1993).
DOI: 10.1594/pangaea.928000
title: M/S Silja Serenade (Helsinki-Stockholm) pCO2 underway measurements in 2018-09

description: Quality control:Measurements during calibration, cleaning, maintenance and low discharge have been removed.-----Flag system:A flag system is applied to the data. Good data that passes the flag control, gets the flag of 11111111. If the raw CO2 partial pressure (not calibration corrected) is out of boundaries (20-1200 ppm), the first digit changes to 9, i.e. if this is only abnormality, the flag would be 9111111. All flags and their boundary limits are listed in the table below.--Flag =&gt; Parameter =&gt; Lower boundary to Upper boundary91111111 =&gt; CO2_ppm_wet =&gt; 20 ppm to 2000 ppm19111111 =&gt; T equ =&gt; -1 °C to 30 °C11911111 =&gt; T tech =&gt; -1 °C to 30 °C11191111 =&gt; Salinity =&gt; 5 to 811119111 =&gt; Pressure =&gt; 0.9 to 1.111111911 =&gt; coeff_A/coeff_B/coeff_C =&gt; -50/0.9/-0.0001 to 100/1.3/0.000111111191 =&gt; SHEQ_flow_LPM/LICOR_flow =&gt; 1.0/50 to N/A/N/A11111119 =&gt; Visually inspected bad data-----Calculations:The CO2 molar fraction observed by the LI-840A is denoted as wet CO2 molar fraction (CO2_ppm_wet).--The molar fraction with respect to dry air is calculated as,CO2_ppm_dry = CO2_ppm_wet / (1 - H2O_ppt/1000),where H2O_ppt is the H2O molar fraction measured by the LI-840A.--For each calibration sequence every 4 hour, a 2nd order polynomial function is fitted to the observed and real molar fractions:CO2_ppm_dry_cal_cor = coeff_A + coeff_B * CO2_ppm_dry + coeff_C * (CO2_ppm_dry)^2Polynomial coefficients (coeff_A, coeff_B and coeff_C) are interpolated between the calibrations.--CO2 partial pressure in dry air is calculated as,pCO2_uatm_dry = CO2_ppm_dry_cal_cor * P_eq_atm--The CO2 partial pressure in wet air (Dickson and Goyet, 1994),pCO2_uatm = pCO2_uatm_dry * (1 - Pws_eq_atm)where saturation water vapor pressure, Pws_eq_atm, is calculated from equilibratortemperature, T_eq_degC (Wagner and PruB, 2002, Eq. 2.5).--Temperature corrected CO2 partial pressure is given for the inlet,pCO2_uatm_temp_corr = pCO2_uatm * exp [ A* (T_in_degC - T_eq_degC)]where A = 0.0423 (Takahashi et al., 1993).
DOI: 10.25549/uschist-ouc110732406
title: Daily Trojan, vol. 41, no. 28, Oct 18, 1949

description: Southern California Daily Trojan, vol. 41, no. 28, October 18, 1949.