Alexey Fedorov
· Professor of Ocean and Atmospheric SciencesYale University · Department of Earth and Planetary Sciences
Active 1998–2025
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About
Alexey Fedorov is a Professor of Oceanic and Atmospheric Sciences in the Department of Earth and Planetary Sciences at Yale University and serves as a Senior Visiting Scientist at the LOCEAN/IPSL at Sorbonne University. His research aims to advance understanding of climate, ocean, and atmospheric dynamics in the context of contemporary global warming and past climate changes. He specializes in the problems of ocean and atmospheric general circulation, large-scale ocean-atmosphere interactions, climate predictability, and mechanisms of long-term climate variations. His group employs modern observational and numerical methodologies, including state-of-the-art general circulation models (GCMs), advanced theoretical methods, statistical data analysis, and conceptual climate models, to investigate physical processes that control climate and improve climate prediction. Fedorov's work encompasses a broad range of topics such as El Niño phenomena, Atlantic meridional overturning circulation (AMOC), ocean circulation and thermal structure, tropical cyclones, and the impacts of climate change on these systems. His contributions include investigating the effects of climate change on El Niño, understanding rapid climate shifts related to ocean circulation reorganizations, and studying the ocean's thermal structure through Lagrangian models. He has been recognized with awards such as the Packard Fellowship in Science and Engineering, the Guggenheim Fellowship, and the Presidential…
Research topics
- Oceanography
- Geology
- Environmental science
- Climatology
Selected publications
Climate impacts of a weakened Atlantic Meridional Overturning Circulation in a warming climate
Science Advances · 2020 · 313 citations
While the Atlantic Meridional Overturning Circulation (AMOC) is projected to slow down under anthropogenic warming, the exact role of the AMOC in future climate change has not been fully quantified. Here, we present a method to stabilize the AMOC intensity in anthropogenic warming experiments by removing fresh water from the subpolar North Atlantic. This method enables us to isolate the AMOC climatic impacts in experiments with a full-physics climate model. Our results show that a weakened AMOC…
Reviews of Geophysics · 2025-03-01 · 32 citations
articleOpen accessAbstract The recharge oscillator (RO) is a simple mathematical model of the El Niño Southern Oscillation (ENSO). In its original form, it is based on two ordinary differential equations that describe the evolution of equatorial Pacific sea surface temperature and oceanic heat content. These equations make use of physical principles that operate in nature: (a) the air‐sea interaction loop known as the Bjerknes feedback, (b) a delayed oceanic feedback arising from the slow oceanic response to wind…
Impacts of Atlantic meridional overturning circulation weakening on Arctic amplification
Proceedings of the National Academy of Sciences · 2024-09-16 · 16 citations
articleOpen accessEnhanced warming of the Arctic region relative to the rest of the globe, known as Arctic amplification, is caused by a variety of diverse factors, many of which are influenced by the Atlantic meridional overturning circulation (AMOC). Here, we quantify the role of AMOC changes in Arctic amplification throughout the twenty-first century by comparing two suites of climate model simulations under the same climate change scenario but with two different AMOC states: one with a weakened AMOC and anoth…
Widening of Wind Stress Anomalies Amplifies ENSO in a Warming Climate
Journal of Climate · 2024-11-04 · 7 citations
articleOpen accessAbstract Climate change simulations generally indicate the strengthening of El Niño–Southern Oscillation (ENSO) sea surface temperature (SST) variability through the twenty-first century, yet a robust physical mechanism explaining this change across different models is still lacking, and the projections for ENSO amplitude exhibit a large spread. Most commonly, changes in the background state of the tropical Pacific are invoked to explain these changes of ENSO. Here, we show that changes in the s…
Tropical Indian Ocean drives Hadley circulation change in a warming climate
National Science Review · 2024-10-22 · 6 citations
articleOpen accessThe weakening and poleward expansion of the Hadley circulation (HC) are considered robust responses of atmospheric meridional circulation to anthropogenic warming. Climate impacts arising from these changes enhance drought conditions and reduce food production in the affected regions. Therefore, understanding the mechanisms of HC changes is critical to anticipating the resultant climate risks. First, we demonstrate that robust future HC changes in boreal winter, and the uncertainty in their futu…
Recent grants
NSF · $368k · 2014–2017
NSF · $289k · 2018–2021
NSF · $324k · 2021–2026
Frequent coauthors
- 206 shared
Brady Ferster
Centre National de la Recherche Scientifique
- 168 shared
Éric Guilyardi
Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques
- 155 shared
Emmanuel Mignot
Stanford University
- 60 shared
Chris Brierley
- 53 shared
K. T. Lawrence
Providence College
- 52 shared
Zhonghui Liu
University of Hong Kong
- 51 shared
Yong Sun
China Southern Power Grid (China)
- 51 shared
Timothy D. Herbert
Education
Ph.D., Scripps Institution of Oceanography
University of California San Diego
Awards & honors
- Packard Fellowship in Science and Engineering (2007-2014)
- Guggenheim Fellowship (2018)
- Presidential climate change research award of the “Make our…
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