goship2015leg1p16n blogspot.com

US GO-SHIP P16N

Thursday, May 14, 2015. The surface ocean has takes up about a quarter of human-emitted carbon dioxide since the start of the industrial revolution. We know this, in part, because of the massive efforts. To quantify the air-sea exchange of carbon dioxide. Both of the circulation and biological feedbacks play a role in the interannual variability of air-sea gas exchange that we observe in the ocean. Looking at the Lamont-Doherty Earth Observatory surface ocean CO2 climatology. LDEO surface CO2 climatology.

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LINKS TO WEB SITE

US Repeat Hydrography Program

See a schedule of cruises, links to data, and PIs for the sample programs on each cruise. See how we do what we do! See a list of publications using US Repeat Hydrography Data. See the guiding policies of the US Repeat Hydrography Program. See the policies and PI contact information. See a map of where repeat hydrography cruises are done. Arctic Geotraces 2015 Chief Scientists Weekly Report 1.

CLIVARGO-SHIP P16N 2015 - Leg 2

Sunday, June 28, 2015. Entering Strait of Juan de Fuca. Final post by Yours Truly, Sabine Mecking. Approaching Port Angeles at 2am. Thursday, June 25, 2015.

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US GO-SHIP P16N

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Thursday, May 14, 2015. The surface ocean has takes up about a quarter of human-emitted carbon dioxide since the start of the industrial revolution. We know this, in part, because of the massive efforts. To quantify the air-sea exchange of carbon dioxide. Both of the circulation and biological feedbacks play a role in the interannual variability of air-sea gas exchange that we observe in the ocean. Looking at the Lamont-Doherty Earth Observatory surface ocean CO2 climatology. LDEO surface CO2 climatology.

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This web page goship2015leg1p16n.blogspot.com states the following, "Thursday, May 14, 2015." We saw that the webpage said " The surface ocean has takes up about a quarter of human-emitted carbon dioxide since the start of the industrial revolution." It also said " We know this, in part, because of the massive efforts. To quantify the air-sea exchange of carbon dioxide. Both of the circulation and biological feedbacks play a role in the interannual variability of air-sea gas exchange that we observe in the ocean. Looking at the Lamont-Doherty Earth Observatory surface ocean CO2 climatology."

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