Simultaneous Hot and Dry Extreme‐Events Increase Wetland Methane Emissions: An Assessment of Compound Extreme‐Event Impacts Using Ameriflux and FLUXNET‐CH$_{\textrm{4}}$ Site Data Sets. Lippmann, T. J. R., Van Der Velde, Y., Naudts, K., Hensgens, G., Vonk, J. E., & Dolman, H. Global Biogeochemical Cycles, 38(9):e2024GB008201, September, 2024.
Simultaneous Hot and Dry Extreme‐Events Increase Wetland Methane Emissions: An Assessment of Compound Extreme‐Event Impacts Using Ameriflux and FLUXNET‐CH$_{\textrm{4}}$ Site Data Sets [link]Paper  doi  abstract   bibtex   
Abstract Wetlands are the largest natural source of global atmospheric methane (CH 4 ). Despite advances to our understanding of changes in temperature and precipitation extremes, their impacts on carbon‐rich ecosystems such as wetlands, remain significantly understudied. Here, we quantify the impacts of extreme temperature, precipitation, and dry events on wetland CH 4 dynamics by investigating the effects of both compound and discrete extreme‐events. We use long‐term climate data to identify extreme‐events and 45 eddy covariance sites data sets sourced from the FLUXNET‐CH 4 database and Ameriflux project to assess impacts on wetland CH 4 emissions. These findings reveal that compound hot + dry extreme‐events lead to large increases in daily CH 4 emissions. However, per event, discrete dry‐only extreme‐events cause the largest total decrease in CH 4 emissions, due to their long duration. Despite dry‐only extreme‐events leading to an overall reduction in CH 4 emissions, enhanced fluxes are often observed for the first days of dry‐only extreme‐events. These effects differ depending on wetland type, where marsh sites tend to be sensitive to most types of extreme‐events. Lagged impacts are significant for at least the 12 months following several types of extreme‐events. These findings have implications for understanding how extreme‐event impacts may evolve in the context of climate change, where changes in the frequency and intensity of temperature and precipitation extreme‐events are already observed. With increasing occurrences of enhanced CH 4 fluxes in response to hot‐only extreme‐events and hot + wet extreme‐events and fewer occurrences of reduced CH 4 fluxes during cold‐only extreme‐events, the impact of wetland CH 4 emissions on climate warming may be increasing. , Key Points Compound extreme‐events (e.g., hot + dry extreme‐events) cause large impacts on daily CH 4 emissions relative to discrete extreme‐events Dry‐only extreme‐events show large total decreases in CH 4 emissions due to the long duration of events, despite initial flux increases Lagged impacts are significant for at least the 12 months following most types of extreme‐events
@article{lippmann_simultaneous_2024,
	title = {Simultaneous {Hot} and {Dry} {Extreme}‐{Events} {Increase} {Wetland} {Methane} {Emissions}: {An} {Assessment} of {Compound} {Extreme}‐{Event} {Impacts} {Using} {Ameriflux} and {FLUXNET}‐{CH}$_{\textrm{4}}$ {Site} {Data} {Sets}},
	volume = {38},
	issn = {0886-6236, 1944-9224},
	shorttitle = {Simultaneous {Hot} and {Dry} {Extreme}‐{Events} {Increase} {Wetland} {Methane} {Emissions}},
	url = {https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2024GB008201},
	doi = {10.1029/2024GB008201},
	abstract = {Abstract
            
              Wetlands are the largest natural source of global atmospheric methane (CH
              4
              ). Despite advances to our understanding of changes in temperature and precipitation extremes, their impacts on carbon‐rich ecosystems such as wetlands, remain significantly understudied. Here, we quantify the impacts of extreme temperature, precipitation, and dry events on wetland CH
              4
              dynamics by investigating the effects of both compound and discrete extreme‐events. We use long‐term climate data to identify extreme‐events and 45 eddy covariance sites data sets sourced from the FLUXNET‐CH
              4
              database and Ameriflux project to assess impacts on wetland CH
              4
              emissions. These findings reveal that compound hot + dry extreme‐events lead to large increases in daily CH
              4
              emissions. However, per event, discrete dry‐only extreme‐events cause the largest total decrease in CH
              4
              emissions, due to their long duration. Despite dry‐only extreme‐events leading to an overall reduction in CH
              4
              emissions, enhanced fluxes are often observed for the first days of dry‐only extreme‐events. These effects differ depending on wetland type, where marsh sites tend to be sensitive to most types of extreme‐events. Lagged impacts are significant for at least the 12 months following several types of extreme‐events. These findings have implications for understanding how extreme‐event impacts may evolve in the context of climate change, where changes in the frequency and intensity of temperature and precipitation extreme‐events are already observed. With increasing occurrences of enhanced CH
              4
              fluxes in response to hot‐only extreme‐events and hot + wet extreme‐events and fewer occurrences of reduced CH
              4
              fluxes during cold‐only extreme‐events, the impact of wetland CH
              4
              emissions on climate warming may be increasing.
            
          , 
            Key Points
            
              
                
                  
                    Compound extreme‐events (e.g., hot + dry extreme‐events) cause large impacts on daily CH
                    4
                    emissions relative to discrete extreme‐events
                  
                
                
                  
                    Dry‐only extreme‐events show large total decreases in CH
                    4
                    emissions due to the long duration of events, despite initial flux increases
                  
                
                
                  Lagged impacts are significant for at least the 12 months following most types of extreme‐events},
	language = {en},
	number = {9},
	urldate = {2024-11-26},
	journal = {Global Biogeochemical Cycles},
	author = {Lippmann, T. J. R. and Van Der Velde, Y. and Naudts, K. and Hensgens, G. and Vonk, J. E. and Dolman, H.},
	month = sep,
	year = {2024},
	pages = {e2024GB008201},
}
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