Time of Emergence and Large Ensemble Intercomparison for Ocean Biogeochemical Trends-Reference-Cited by-同舟云学术

Time of Emergence and Large Ensemble Intercomparison for Ocean Biogeochemical Trends

Published:2020-08 Issue:8 Volume:34 Page:
ISSN:0886-6236
Container-title:Global Biogeochemical Cycles
language:en
Short-container-title:Global Biogeochem. Cycles

Author:

Schlunegger Sarah¹^ORCID,Rodgers Keith B.¹²³^ORCID,Sarmiento Jorge L.¹^ORCID,Ilyina Tatiana⁴^ORCID,Dunne John P.⁵^ORCID,Takano Yohei⁴⁶^ORCID,Christian James R.⁷,Long Matthew C.⁸^ORCID,Frölicher Thomas L.⁹¹⁰^ORCID,Slater Richard¹^ORCID,Lehner Flavio⁸^ORCID

Affiliation:

1. Program in Atmospheric and Oceanic Sciences Princeton University Princeton NJ USA

2. Center for Climate Physics Institute for Basic Science Busan South Korea

3. Pusan National University Busan South Korea

4. Max Plank Institute for Meteorology Hamburg Germany

5. NOAA Geophysical Fluid Dynamics Laboratory Princeton NJ USA

6. Los Alamos National Laboratory Los Alamos NM USA

7. Canadian Center for Climate Modeling and Analysis Victoria British Columbia Canada

8. National Center for Atmospheric Research Boulder CO USA

9. Climate and Environmental Physics, Physics Institute University of Bern Bern Switzerland

10. Oeschger Centre for Climate Change Research University of Bern Bern Switzerland

Funder

National Oceanic and Atmospheric Administration

Horizon 2020

National Aeronautics and Space Administration

National Science Foundation

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

Publisher

American Geophysical Union (AGU)

Subject

Atmospheric Science,General Environmental Science,Environmental Chemistry,Global and Planetary Change

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019GB006453

Reference59 articles.

1. Carbon emission limits required to satisfy future representative concentration pathways of greenhouse gases

2. Carbon–Concentration and Carbon–Climate Feedbacks in CMIP5 Earth System Models

3. Sea surface salinity measurements in the historical database

4. Using a large ensemble of simulations to assess the Northern Hemisphere stratospheric dynamical response to tropical volcanic eruptions and its uncertainty

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