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

Abstract

Abstract. 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 NPP estimates and large ensemble simulation output of two widely-used and comprehensive Earth system models, GFDL-ESM2M-LE and 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 three times higher (more than 10 days per year) than if MHWs (temperature above the 90th percentile threshold) and NPPX events (NPP below the 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 days per year), but relatively frequent in CESM2-LE. In the Southern Ocean south of 60° 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° S and 50° 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.

Understanding the compound marine heatwave and low-chlorophyll extremes in the western Pacific Ocean

“…For example, Noh et al (2022) reported that MHWs typically reduce Chl in the tropical and subtropical regions, where background nitrate concentrations are insufficient. Le Grix et al (2021) discovered frequent compound MHW-LChl events in the central equatorial Pacific and Indian Ocean, which corresponds to the co-occurrence of MHWs and low net primary productivity events (Le Grix et al, 2022). However, the features of compound MHW-LChl events over the marginal seas are not revealed in Le Grix et al (2021), we perform a more detailed analysis of multi-scale characteristics of compound MHW-LChl extremes over the western Pacific Ocean, including the marginal seas regions.…”

Large potential impacts of marine heatwaves on ecosystem functioning

“…The study of the relationships between extreme events (e.g., compound events) is very recent (Gruber et al., 2021; Le Grix et al., 2022), and there are still many questions to be answered about their interactions and functioning at the physical level, in particular the quantification of the decrease in NPP associated with MHWs of different intensity and occurring at different locations. Thus, it seemed extremely ambitious to address this issue at the biological level, so we chose to free ourselves from this relationship and thus fixed net primary production in our simulations.…”

“…However, associated with MHWs, as under global warming, the abrupt increase in temperature causes an increase in surface water stratification and changes in nutrient availability. At low latitudes, MHWs could be associated with a decrease in nutrients at the ocean surface and, thus, a decrease in phytoplankton growth, leading to an extreme drop in primary production (Le Grix et al, 2022). These two extreme events could have an additional or synergic negative effect on the functioning and stability of marine ecosystems with cascading impacts through the food web depending on which types of phytoplankton marine species prefer to graze on (Bindoff et al, 2019;Cavole et al, 2016;Cheung & Frölicher, 2020).…”

Column-Compound Extremes in the Global Ocean

“…E. Smith et al, 2023). But also ocean acidity extremes (OAX) (Hauri et al, 2013;Kwiatkowski & Orr, 2018;Negrete-García et al, 2019;Burger et al, 2020;Desmet et al, 2022) and low oxygen extremes (LOX) (Chan et al, 2008;Hofmann et al, 2011;Köhn et al, 2022) are receiving increasing attention, with the study of compound marine extremes, that is, events when conditions are extreme in more than one stressor emerging as an -2-manuscript submitted to AGU Advances issue of special concern (Gruber et al, 2021;Le Grix et al, 2021;Burger et al, 2022;Le Grix et al, 2022). Such compounded extreme events can have a disproportionately large impact on marine biota, especially when the different stressors act synergistically, that is, when they reinforce each other (Crain et al, 2008;Boyd & Brown, 2015;Pirotta et al, 2022).…”