Externally funded research projects (to be updated):
Current: The impacts of stratospheric temperature on atmospheric and oceanic circulation and Atlantic Multidecadal Variability. A manuscript is under review in Journal of Climate.
2023-2026: co-Principal Investigator, “ The role of tropical Indian Ocean warming in E3SM and other Earth system models”. (Collaboration with Duke University). Department of Energy
2022-2025: Principal Investigator, “The mechanisms, impacts and predictability of extreme El Niño events in E3SM and other Earth system models”. (Collaboration with Harvard University).
2022-2023: PI, Yale Planetary Solutions seed grant: “Simulating Pliocene climate 2022–2023 as a blueprint for future warming: From cloud physics and ocean circulation to extreme precipitation and droughts”
2021-2024: Principal Investigator, “Coupled dynamics of the North equatorial countercurrent and the Intertropical convergence zone”. NASA
2021-2024: PI, “Collaborative research: the impacts of the Atlantic meridional overturning circulation in a warming climate”. NSF
2020-2023: Principal Investigator. , “Changes in the mean state of the tropical Pacific and the mechanisms of extreme El Niño events”. NOAA
2019-2025: co-Investigator, “Arctic climate change, global ocean circulation and basin interconnections”. at LOCEAN/IPSL, Sorbonne University, France
2018-2021: Principal Investigator , ”Collaborative research: Examining the links between AMOC variability and Atlantic Multidecadal Variability (AMV) – from oceanic internal modes to climate impacts”. NSF
2017-2020: Principal Investigator, “The Arctic ocean control of the Atlantic meridional overturning circulation on multi-decadal and longer timescales”. NSF
2011-2014: Principal Investigator, “A Generalized Stability Analysis of the AMOC in Earth System Models: Implications for Decadal Variability and Abrupt Climate Change.” Department of Energy.
2011-2014: Co-Principal Investigator, “Collaboration Research: Lagrangian Modeling of Convectively Coupled Equatorial Waves and the Madden Julian Oscillation.” National Science Foundation.
2009-2012: Principal Investigator, “Collaboration Research: Reconstructing Meridional Temperature Gradient and Climate Conditions of the Early Pliocene.” National Science Foundation.
2009-2011: Principal Investigator, “Stability of the Atlantic Meridional Overturning Circulation.” Department of Energy.
2007-2014: Principal Investigator. “El Niño and Global Warming: Past and Future Response of the Atmosphere-Ocean System.” David and Lucile Packard Foundation.
2006-2008: Principal Investigator, “Net Energy Dissipation in the Tropical Ocean and ENSO Dynamics: modeling and theoretical study.” National Science Foundation.
2006-2008: Principal Investigator, “Abrupt Climate Changes Involving the Tropics.” Department of Energy.
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Fig. 1: El Niño events of 1965/1966 and 1982/1983 shown as warm sea surface
temperature anomalies propagating along the equator (Fedorov and Philander 2000, 2001)
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Fig. 2: Different states of the Atlanitc ocean meridional overturning
circulation (AMOC) in an idealized ocean model (Fedorov et al 2007)
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Fig. 3: Interdecadal mode of the AMOC in an ocean GCM (Sevellec and Fedorov 2013)