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KPDC, Korea Polar Data Center

Korea Polar Data Center Scientific observations and results from Antarctica shall
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Distribution of total alkalinity in the Chukchi Sea of the Arctic Ocean in summer 2012.

As a part of the 2012 Korea-Polar Ocean Rapid Transition (K-PORT) program, the IBRV Araon occupied 44 hydrographic stations in the Chukchi Borderland and Medeleev Ridge of the Arctic Ocean from August 1 to September 10. In order to study for rapid climate changes and its impact on distribution of the inorganic CO2 system, 354 samples for total alkalinity (TA) were taken from Niskin bottle to 500 ml boro-silicate glass bottles on board. Accurate measurement concerning spatio-temporal variability in CO2 in the water column is highly important to understanding of global carbon cycle and reliable prediction for the future atmospheric concentration of CO2. From flux study perspective of CO2, the Arctic Ocean has known as sink for atmospheric CO2. But there wasn't enough data, and sea ice have an ambiguous role of air-sea CO2 exchange so that further research must be conducted.

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Entry ID
KOPRI-KPDC-00000436
KPDC_DTAS_ARCTIC_2012_01 (Old ID)
DOI
https://dx.doi.org/doi:10.22663/KOPRI-KPDC-00000436.1
Science Keyword
EARTH SCIENCE > Oceans > Ocean Chemistry > Carbon Dioxide
EARTH SCIENCE > Atmosphere > Atmospheric Chemistry > Carbon and Hydrocarbon Compounds > Carbon Dioxide
ISO Topic
CLIMATOLOGY/METEOROLOGY/ATMOSPHERE
Platform
ARAON (Icebreaker Research Vessel, KOPRI)
Instrument
VINDTA(Versatile Instrument for Determination of Titration Alkalinity)
Personnel
Tae Siek Rhee (rhee@kopri.re.kr)
Project
PM12020, Korea Polar Ocean in Rapid Transition. PI.Sung-Ho Kang
Research period
2012-08-01 - 2012-09-10
Create/Update Date
2013-08-26 00:00:00 UTC
Location
Continent > North America > United States Of America > Alaska
Ocean > Arctic Ocean > Chukchi Sea
Dataset
Distribution of total alkalinity in the Chukchi Sea of the Arctic Ocean in summer 2012. Korea Polar Ocean in Rapid Transition Tae Siek Rhee
Citation
The data(KOPRI-KPDC-00000436) used in this work was provided by the Korea Polar Research Institute.

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