CLIVAR-FIO BGC Summer School Reading and Instructions
CLIVAR-FIO BGC Summer School Reading List
- DeVries, T., 2022: The Ocean Carbon Cycle. Annual Review of Environment and Resources, 47: 317-41
- Kang, X., R.-H. Zhang, C. Gao, J. Zhu, 2017: An improved ENSO simulation by representing chlorophyll-induced climate feedback in the NCAR Community Earth System Model. Scientific Reports, 7, doi:10.1038/s41598-017-17390-2
- Mao, S.-H., H.-H. Zhang, G.-C. Zhuang, et al. 2022: Aerobic oxidation of methane significatly reduces global diffusive methane emissions from shallow marine waters. Nature Communications, 13:7309, doi:10.1038/s414670922035082-y.
- Mao, S.-H., J.-Y. Wang, S. Joye, G.-C. Zhuang, 2024: Marine methane paradox: Enigmatic production of methane in oxygenated waters. The Innovation Geoscience, 2(2): 100071.
- McGillicuddy Jr., D. J., Mechanisms of physical-biological-biogeochemical interaction at the oceanic mesoscale. Annual Review of Marine Science, 8:125-159.
- Montes, I., B. Dewitte, E. Gutknecht, et al. 2014: High-resolution modeling of the Eastern Tropical Pacific oxygen minimum zone: Sensitivity to the tropical oceanic circulation. J. Geophysical Research Oceans, 119, 5515-5532, doi:10.1002/2014JC009858.
- Rohr, T., A. J. Richardson, A. Lenton, M. Chamberlain, E. H. Shadwick, 2023: Zooplankton grazing is the largest source of uncertainty for marine carbon cycling in CMIP6 models. 4:212, doi: 10.1038/s43247-023-00871-w.
- Zhang, R.-H., 2015: An ocean-biology-induced negative feedback on ENSO as derived from a hybrid coupled model of the tropical Pacific. J. Geophysical Research Oceans, 120, 8052-8076, doi:10.1002/2015JC011305.
- Zhang, R.-H., F. Tian, X. Wang, 2018: A new hybrid coupled model of atmosphere, ocean physics, ad ocean biogeochemistry to represent biogeophysical feedback effects in the tropical Pacific. J. Advances in Modeling Earth Systems, 10, 8, 1901-1923, doi::10.1029/2017MS001250.
- Zhang, R.-H., F. Tian, H. Zhi, X. Kang, 2019: Observed structural relationships between ocean chlorophyll variability and its heating effects on the ENSO. Climate Dynamics, doi:10.1007/s00382-019-04844-8.
