Future Changes in the Intensity and Duration of Marine Heat and Cold Waves: Insights from Coupled Model Initial-Condition Large Ensembles

Deser, Clara; Phillips, Adam S.; Alexander, Michael. A.; Amaya, Dillon J.; Capotondi, Antonietta; Jacox, Michael G.; Scott, James D.

doi:10.1175/jcli-d-23-0278.1

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Future Changes in the Intensity and Duration of Marine Heat and Cold Waves: Insights from Coupled Model Initial-Condition Large Ensembles

2024
By Deser, Clara ; Phillips, Adam S. ; Alexander, Michael. A. ; ...

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Journal Title:

Journal of Climate
Personal Author:

Deser, Clara ; Phillips, Adam S. ; Alexander, Michael. A. ; Amaya, Dillon J. ; Capotondi, Antonietta ; Jacox, Michael G. ; Scott, James D.
NOAA Program & Office:

NMFS (National Marine Fisheries Service) ; OAR (Oceanic and Atmospheric Research) ; CIRES (Cooperative Institute for Research in Environmental Sciences) ; PSL (Physical Sciences Laboratory) ; SWFSC (Southwest Fisheries Science Center)
Description:

The future evolution of sea surface temperature (SST) extremes is of great concern, not only for the health of marine ecosystems and sustainability of commercial fisheries, but also for precipitation extremes fueled by moisture evaporated from the ocean. This study examines the projected influence of anthropogenic climate change on the intensity and duration of monthly SST extremes, hereafter termed marine heat waves (MHWs) and marine cold waves (MCWs), based on initial-condition large ensembles with seven Earth system models. The large number of simulations (30–100) with each model allows for robust quantification of future changes in both the mean state and variability in each model. In general, models indicate that future changes in variability will cause MHW and MCW events to intensify in the northern extratropics and weaken in the tropics and Southern Ocean, and to shorten in duration in many areas. These changes are generally symmetric between MHWs and MCWs, except for the longitude of duration change in the tropical Pacific and sign of duration change in the Arctic. Projected changes in ENSO account for a large fraction of the variability-induced changes in MHW and MCW characteristics in each model and are responsible for much of the intermodel spread as a result of differences in future ENSO behavior. The variability-related changes in MHW and MCW characteristics noted above are superimposed upon large mean-state changes. Indeed, their contribution to the total change in SST during MHW and MCW events is generally <10% except in polar regions where they contribute upward of 50%.
Source:

Journal of Climate, 37(6), 1877-1902
DOI:

https://doi.org/10.1175/jcli-d-23-0278.1
ISSN:

0894-8755 ; 1520-0442
Format:

pdf
Publisher:

American Meteorological Society
Document Type:

Journal Article
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Other
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Library
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urn:sha-512:d0741f1ef93525879a634fb253566e2b78b867523896023a1c0dfc7ce22efb3cbacd8a097b42fa488df93d186c3e67a538eac9a804ab4a7f8646091d57be1af4
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https://repository.library.noaa.gov/view/noaa/69316/noaa_69316_DS1.pdf
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[PDF - 11.43 MB ]

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