Characterizing Transport between the Surface Mixed Layer and the Ocean Interior with a Forward and Adjoint Global Ocean Transport Model

By F. Primeau. 2005

161 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/032b104d35984e1fe6e2699d71ff8f738d415e7d

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. M. Horner‐Devine
2. Jonathan A. Eisen
3. R. Benner
4. G. Kattner
5. Steven W. Wilhelm
6. S. Allison
7. K. Penn
8. U. Passow

In Oceanography

1. C. Carlson
2. M. Weinbauer
3. U. Passow
4. G. Herndl
5. Dennis A. Hansell
6. Farooq Azam
7. G. Kattner
8. David L. Kirchman

Citations in the corpus

• The biological pump in a high CO 2 world (2012, background): “This criterion is met after carbon is transported below 1000 m on average (Primeau 2005) and coincides with the nitrate maximum, the base of the mesopelagic zone, and the greatest extent of vertically migrating zooplankton.”
• Drivers of bacterial β-diversity depend on spatial scale (2011, methodology): “To estimate the dispersal time of a hypothetical microbial cell between each sampling location, we used a global ocean circulation model (23) as applied previously in Martiny et al.”
• Microbial production of recalcitrant dissolved organic matter: long-term carbon storage in the global ocean (2010, background): “This age is higher than the turnover time of the thermohaline circulation (550–2,000 years”