Hotspots and drivers of compound marine heatwaves and low net primary production extremes

<p>Extreme events can severely impact marine organisms and ecosystems. Of particular concern are multivariate compound events, namely when conditions are simultaneously extreme for multiple ocean ecosystem stressors. In 2013–2015 for example, an extensive marine heatwave (MHW), known as the Bl...

Full description

Bibliographic Details
Main Authors: N. Le Grix, J. Zscheischler, K. B. Rodgers, R. Yamaguchi, T. L. Frölicher
Format: Article
Language:English
Published: Copernicus Publications 2022-12-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/19/5807/2022/bg-19-5807-2022.pdf
_version_ 1797980501688975360
author N. Le Grix
N. Le Grix
J. Zscheischler
J. Zscheischler
J. Zscheischler
K. B. Rodgers
K. B. Rodgers
R. Yamaguchi
R. Yamaguchi
R. Yamaguchi
T. L. Frölicher
T. L. Frölicher
author_facet N. Le Grix
N. Le Grix
J. Zscheischler
J. Zscheischler
J. Zscheischler
K. B. Rodgers
K. B. Rodgers
R. Yamaguchi
R. Yamaguchi
R. Yamaguchi
T. L. Frölicher
T. L. Frölicher
author_sort N. Le Grix
collection DOAJ
description <p>Extreme events can severely impact marine organisms and ecosystems. Of particular concern are multivariate compound events, namely when conditions are simultaneously extreme for multiple ocean ecosystem stressors. In 2013–2015 for example, an extensive marine heatwave (MHW), known as the Blob, co-occurred locally with extremely low net primary productivity (NPPX) and negatively impacted marine life in the northeast Pacific. Yet, little is known about the characteristics and drivers of such multivariate compound MHW–NPPX events. Using five different satellite-derived net primary productivity (NPP) estimates and large-ensemble-simulation output of two widely used and comprehensive Earth system models, the Geophysical Fluid Dynamics Laboratory (GFDL) ESM2M-LE and Community Earth System Model version 2 (CESM2-LE), we assess the present-day distribution of compound MHW–NPPX events and investigate their potential drivers on the global scale. The satellite-based estimates and both models reveal hotspots of frequent compound events in the center of the equatorial Pacific and in the subtropical Indian Ocean, where their occurrence is at least 3 times higher (more than 10 d yr<span class="inline-formula"><sup>−1</sup></span>) than if MHWs (temperature above the seasonally varying 90th-percentile threshold) and NPPX events (NPP below the seasonally varying 10th-percentile threshold) were to occur independently. However, the models show disparities in the northern high latitudes, where compound events are rare in the satellite-based estimates and GFDL ESM2M-LE (less than 3 d yr<span class="inline-formula"><sup>−1</sup></span>) but relatively frequent in CESM2-LE. In the Southern Ocean south of 60<span class="inline-formula"><sup>∘</sup></span> S, low agreement between the observation-based estimates makes it difficult to determine which of the two models better simulates MHW–NPPX events. The frequency patterns can be explained by the drivers of compound events, which vary among the two models and phytoplankton types. In the low latitudes, MHWs are associated with enhanced nutrient limitation on phytoplankton growth, which results in frequent compound MHW–NPPX events in both models. In the high latitudes, NPPX events in GFDL ESM2M-LE are driven by enhanced light limitation, which rarely co-occurs with MHWs, resulting in rare compound events. In contrast, in CESM2-LE, NPPX events in the high latitudes are driven by reduced nutrient supply that often co-occurs with MHWs, moderates phytoplankton growth, and causes biomass to decrease. Compound MHW–NPPX events are associated with a relative shift towards larger phytoplankton in most regions, except in the eastern equatorial Pacific in both models, as well as in the northern high latitudes and between 35 and 50<span class="inline-formula"><sup>∘</sup></span> S in CESM2-LE, where the models suggest a shift towards smaller phytoplankton, with potential repercussions on marine ecosystems. Overall, our analysis reveals that the likelihood of compound MHW–NPPX events is contingent on model representation of the factors limiting phytoplankton production. This identifies an important need for improved process understanding in Earth system models used for predicting and projecting compound MHW–NPPX events and their impacts.</p>
first_indexed 2024-04-11T05:56:16Z
format Article
id doaj.art-4fb6390ad5f3457c9becddd92bf513eb
institution Directory Open Access Journal
issn 1726-4170
1726-4189
language English
last_indexed 2024-04-11T05:56:16Z
publishDate 2022-12-01
publisher Copernicus Publications
record_format Article
series Biogeosciences
spelling doaj.art-4fb6390ad5f3457c9becddd92bf513eb2022-12-22T04:41:53ZengCopernicus PublicationsBiogeosciences1726-41701726-41892022-12-01195807583510.5194/bg-19-5807-2022Hotspots and drivers of compound marine heatwaves and low net primary production extremesN. Le Grix0N. Le Grix1J. Zscheischler2J. Zscheischler3J. Zscheischler4K. B. Rodgers5K. B. Rodgers6R. Yamaguchi7R. Yamaguchi8R. Yamaguchi9T. L. Frölicher10T. L. Frölicher11Climate and Environmental Physics, Physics Institute, University of Bern, Bern, SwitzerlandOeschger Centre for Climate Change Research, University of Bern, Bern, SwitzerlandClimate and Environmental Physics, Physics Institute, University of Bern, Bern, SwitzerlandOeschger Centre for Climate Change Research, University of Bern, Bern, SwitzerlandDepartment of Computational Hydrosystems, Helmholtz Centre for Environmental Research – UFZ, Leipzig, GermanyCenter for Climate Physics, Institute for Basic Science, Busan, South KoreaPusan National University, Busan, South Korea​​​​​​​Center for Climate Physics, Institute for Basic Science, Busan, South KoreaPusan National University, Busan, South Korea​​​​​​​Research Institute for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, JapanClimate and Environmental Physics, Physics Institute, University of Bern, Bern, SwitzerlandOeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland<p>Extreme events can severely impact marine organisms and ecosystems. Of particular concern are multivariate compound events, namely when conditions are simultaneously extreme for multiple ocean ecosystem stressors. In 2013–2015 for example, an extensive marine heatwave (MHW), known as the Blob, co-occurred locally with extremely low net primary productivity (NPPX) and negatively impacted marine life in the northeast Pacific. Yet, little is known about the characteristics and drivers of such multivariate compound MHW–NPPX events. Using five different satellite-derived net primary productivity (NPP) estimates and large-ensemble-simulation output of two widely used and comprehensive Earth system models, the Geophysical Fluid Dynamics Laboratory (GFDL) ESM2M-LE and Community Earth System Model version 2 (CESM2-LE), we assess the present-day distribution of compound MHW–NPPX events and investigate their potential drivers on the global scale. The satellite-based estimates and both models reveal hotspots of frequent compound events in the center of the equatorial Pacific and in the subtropical Indian Ocean, where their occurrence is at least 3 times higher (more than 10 d yr<span class="inline-formula"><sup>−1</sup></span>) than if MHWs (temperature above the seasonally varying 90th-percentile threshold) and NPPX events (NPP below the seasonally varying 10th-percentile threshold) were to occur independently. However, the models show disparities in the northern high latitudes, where compound events are rare in the satellite-based estimates and GFDL ESM2M-LE (less than 3 d yr<span class="inline-formula"><sup>−1</sup></span>) but relatively frequent in CESM2-LE. In the Southern Ocean south of 60<span class="inline-formula"><sup>∘</sup></span> S, low agreement between the observation-based estimates makes it difficult to determine which of the two models better simulates MHW–NPPX events. The frequency patterns can be explained by the drivers of compound events, which vary among the two models and phytoplankton types. In the low latitudes, MHWs are associated with enhanced nutrient limitation on phytoplankton growth, which results in frequent compound MHW–NPPX events in both models. In the high latitudes, NPPX events in GFDL ESM2M-LE are driven by enhanced light limitation, which rarely co-occurs with MHWs, resulting in rare compound events. In contrast, in CESM2-LE, NPPX events in the high latitudes are driven by reduced nutrient supply that often co-occurs with MHWs, moderates phytoplankton growth, and causes biomass to decrease. Compound MHW–NPPX events are associated with a relative shift towards larger phytoplankton in most regions, except in the eastern equatorial Pacific in both models, as well as in the northern high latitudes and between 35 and 50<span class="inline-formula"><sup>∘</sup></span> S in CESM2-LE, where the models suggest a shift towards smaller phytoplankton, with potential repercussions on marine ecosystems. Overall, our analysis reveals that the likelihood of compound MHW–NPPX events is contingent on model representation of the factors limiting phytoplankton production. This identifies an important need for improved process understanding in Earth system models used for predicting and projecting compound MHW–NPPX events and their impacts.</p>https://bg.copernicus.org/articles/19/5807/2022/bg-19-5807-2022.pdf
spellingShingle N. Le Grix
N. Le Grix
J. Zscheischler
J. Zscheischler
J. Zscheischler
K. B. Rodgers
K. B. Rodgers
R. Yamaguchi
R. Yamaguchi
R. Yamaguchi
T. L. Frölicher
T. L. Frölicher
Hotspots and drivers of compound marine heatwaves and low net primary production extremes
Biogeosciences
title Hotspots and drivers of compound marine heatwaves and low net primary production extremes
title_full Hotspots and drivers of compound marine heatwaves and low net primary production extremes
title_fullStr Hotspots and drivers of compound marine heatwaves and low net primary production extremes
title_full_unstemmed Hotspots and drivers of compound marine heatwaves and low net primary production extremes
title_short Hotspots and drivers of compound marine heatwaves and low net primary production extremes
title_sort hotspots and drivers of compound marine heatwaves and low net primary production extremes
url https://bg.copernicus.org/articles/19/5807/2022/bg-19-5807-2022.pdf
work_keys_str_mv AT nlegrix hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT nlegrix hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT jzscheischler hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT jzscheischler hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT jzscheischler hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT kbrodgers hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT kbrodgers hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT ryamaguchi hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT ryamaguchi hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT ryamaguchi hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT tlfrolicher hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes
AT tlfrolicher hotspotsanddriversofcompoundmarineheatwavesandlownetprimaryproductionextremes