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McDowell, N. G.

Publications and source records attributed to McDowell, N. G..

2 recordsLinked to original sources

Rising water is an underappreciated driver of forest mortality

Forests are known to burn and desiccate under a changing climate; less appreciated is that they also drown. Across much of the globe, a warming atmosphere is amplifying the length and intensity of both droughts and floods. Whereas massive die-offs from drought and fire are widely studied as consequences of climate change on forests, inundation-induced mortality remains poorly quantified. Using approximately 1 m resolution aerial imagery and deep learning, we tracked over 260 million dead trees across the United States' Great Lakes and ocean coastlines from 2012 to 2023. Within 10 km of the coasts, more than half of mapped mortality was concentrated in just 10% of forests, primarily in high-elevation inland wetlands and low-lying forests prone to inundation. Mortality rates doubled within a decade around expanding freshwater lakes and in inland wetlands experiencing intensifying regional-scale precipitation, while tripling in low-lying coastal forests where salinization compounded inundation in sea-level rise hotspots. Our findings identify rising waters as a widespread, underappreciated driver of forest die-off that can extend far inland, underscoring the need to reassess the impacts of climate change on the functioning, demography, and carbon-methane budgets amongst the world's most carbon-rich forests as seas rise and hydroclimate shifts globally.

ecology↗

Groundwater redox dynamics across the terrestrial-aquatic interface of Lake Erie coastal ecosystems

Groundwater biogeochemistry in coastal areas is spatially and temporally dynamic because fluctuations in groundwater level may cause alternate redox between distinct hydrological conditions. Recent studies have proposed connections between biogeochemistry and large-scale hydrological processes, specifically focusing on the role of redox-active compounds in changing the oxidation state during flooding and draining events. While water saturation generally results in a shift of redox-active compounds from electron donors to acceptors, the specific mechanisms underlying the transition of groundwater between oxidizing and reducing conditions in response to water level fluctuations are uncertain. To determine the effects of groundwater levels on redox dynamics, we monitored groundwater redox potential across the terrestrial-aquatic interface in Lake Erie coastal areas throughout the high and low-water seasons. In contrast to previously observed responses to flooding in soils, our results revealed patterns of oxidizing redox potentials during high-water and reducing during low-water periods. Furthermore, short-term fluctuations in water table levels significantly impacted the redox potential of groundwater when dissolved oxygen increased, and redox dynamics displayed voltage hysteresis in most events. Based on these findings, we propose that for improved predictions of microbial functions and biogeochemical cycles, redox-informed models should incorporate the antagonistic changes in groundwater redox balance compared to soils and consider the time lags in redox fluctuations. O_FIG O_LINKSMALLFIG WIDTH=200 HEIGHT=92 SRC="FIGDIR/small/544684v1_figu1.gif" ALT="Figure 1"> View larger version (26K): org.highwire.dtl.DTLVardef@4d7a19org.highwire.dtl.DTLVardef@8b2b92org.highwire.dtl.DTLVardef@d9bc11org.highwire.dtl.DTLVardef@ca3e13_HPS_FORMAT_FIGEXP M_FIG Graphical AbstractConceptual diagram of groundwater redox fluctuations in coastal ecosystems. Large redox fluctuations are derived by dissolved oxygen inputs and smaller more frequent redox fluctuations are led by redox sensitive species leaching from topsoil. C_FIG

ecology↗