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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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US GO-SHIP P16N | goship2015leg1p16n.blogspot.com Reviews
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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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US GO-SHIP P16N | goship2015leg1p16n.blogspot.com Reviews

https://goship2015leg1p16n.blogspot.com

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.

INTERNAL PAGES

goship2015leg1p16n.blogspot.com goship2015leg1p16n.blogspot.com
1

US GO-SHIP P16N: Traversing the Anomalously Warm Pacific

http://goship2015leg1p16n.blogspot.com/2015/05/traversing-anomalously-warm-pacific.html

Friday, May 1, 2015. Traversing the Anomalously Warm Pacific. Abnormally high Sea Surface Temperatures (SST) anomalies in the North Pacific have been implicated. In the wild weather over the winter in the US midwest and northeast as well as the drought in California and highlighted in the press. Recently. The region of the North Pacific containing this warm water has been dubbed the "Blob" by Washington State Climatologist Nick Bond. IPO), a positive phase of the Pacific Decadal Oscillation (PDO). Has be...

2

US GO-SHIP P16N: Waiting to Exhale....

http://goship2015leg1p16n.blogspot.com/2015/05/waiting-to-exhale.html

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.

3

US GO-SHIP P16N: Sampling

http://goship2015leg1p16n.blogspot.com/2015/05/sampling.html

Tuesday, May 5, 2015. Over and over, we sample. The equatorial transect was the most intense - 4 - 5 stations a day, sometimes with only an hour of CTD time out of the water. We have been exhaling a bit as our stations get further and further apart. One of the crew began comparing us to zombies who crave sea water. "Must sample.need seawater. ". Subscribe to: Post Comments (Atom). Mixing in the Equatorial Pacific Ocean. Color by Number: Ocean Optics. Science Meets Art on the Ronald H. Brown.

4

US GO-SHIP P16N: Mixing in the Equatorial Pacific Ocean

http://goship2015leg1p16n.blogspot.com/2015/05/mixing-in-equatorial-pacific-ocean.html

Wednesday, May 13, 2015. Mixing in the Equatorial Pacific Ocean. Miguel Angel Jimenez-Urias is a 3. Year oceanography graduate student at the University of Washington. His work focuses on the topographic control of fronts at both small and large scales. While his work uses primarily numerical modeling and laboratory experiments, he tries to include observational methods in his projects to advance his academic and professional development. Of course my feelings. This is a simple way of saying that. In the...

5

US GO-SHIP P16N: May 2015

http://goship2015leg1p16n.blogspot.com/2015_05_01_archive.html

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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clivarp16n2015.blogspot.com clivarp16n2015.blogspot.com

CLIVAR/GO-SHIP P16N 2015 - Leg 2 : Getting ready

http://clivarp16n2015.blogspot.com/2015/05/getting-ready.html

CLIVAR/GO-SHIP P16N 2015 - Leg 2. Sunday, May 17, 2015. The last occupation of the P16N Hawaii-Alaska leg took place in March 2006 on the R/V Thompson. Almost a decade later, we are about to head out into the northeastern Pacific again, this time on the R/V Brown. Leg 1 from Tahiti-Hawaii is already complete. See their blog posts here. Picture taken from Bridge of R/V Thompson in 2006, somewhere along 152°W. Posted by Sabine Mecking. Denim and Pool Day. Radiocarbon dating of organic material dissolved i.

ushydro.ucsd.edu ushydro.ucsd.edu

US Repeat Hydrography Program

http://ushydro.ucsd.edu/outreach/content/2015/04/18/p16n-2015-blog

Home U.S. Repeat Hydrography. Cruise Data and Schedules. Go to the P16N Blog. Follow the participants of P16N as they do science in the Central and Northern Pacific. Weekly Report 1 (26.6 KB). Weekly Report 3 (1.6 MB). A Day in the Life. Cruise Data and Schedules.

clivarp16n2015.blogspot.com clivarp16n2015.blogspot.com

CLIVAR/GO-SHIP P16N 2015 - Leg 2 : May 2015

http://clivarp16n2015.blogspot.com/2015_05_01_archive.html

CLIVAR/GO-SHIP P16N 2015 - Leg 2. Sunday, May 31, 2015. Denim and Pool Day. Today was declared denim day (by our newly established science party morale chief) to make everyone look good. The weather has been great, so we also used the new pool (purchased in Hawaii) on the aft deck for the first time. However, as we are constantly heading further north, I suspect that only our die-hard Alaskan participants will be found in the pool in a few days or so. Denim-wearers gathering in the CTD lab. Last view of ...

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goship2015leg1p16n.blogspot.com 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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