Phenological shifts in lake stratification under climate change
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In: Nature Communications, Vol. 12, 2318 (2021), 19.04.2021.
Research output: Contribution to journal › Article › peer-review
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T1 - Phenological shifts in lake stratification under climate change
AU - Woolway, R. Iestyn
AU - Sharma, Sapna
AU - Weyhenmeyer, Gesa A.
AU - Debolskiy, Andrey
AU - Golub, Malgorzata
AU - Mercado-Bettin, Daniel
AU - Perroud, Marjorie
AU - Stepanenko, Victor
AU - Tan, Zeli
AU - Grant, Luke
AU - Ladwig, Robert
AU - Mesman, Jorrit
AU - Moore, Tadhg N.
AU - Shatwell, Tom
AU - Vanderkelen, Inne
AU - Austin, Jay A.
AU - DeGasperi, Curtis L.
AU - Dokulil, Martin
AU - La Fuente, Sofia
AU - Mackay, Eleanor B.
AU - Schladow, S. Geoffrey
AU - Watanabe, Shohei
AU - Marce, Rafael
AU - Pierson, Don C.
AU - Thiery, Wim
AU - Jennings, Eleanor
PY - 2021/4/19
Y1 - 2021/4/19
N2 - One of the most important physical characteristics driving lifecycle events in lakes is stratification. Already subtle variations in the timing of stratification onset and break-up (phenology) are known to have major ecological effects, mainly by determining the availability of light, nutrients, carbon and oxygen to organisms. Despite its ecological importance, historic and future global changes in stratification phenology are unknown. Here, we used a lake-climate model ensemble and long-term observational data, to investigate changes in lake stratification phenology across the Northern Hemisphere from 1901 to 2099. Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 ± 7.0 days earlier and end 11.3 ± 4.7 days later by the end of this century. It is very likely that this 33.3 ± 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.
AB - One of the most important physical characteristics driving lifecycle events in lakes is stratification. Already subtle variations in the timing of stratification onset and break-up (phenology) are known to have major ecological effects, mainly by determining the availability of light, nutrients, carbon and oxygen to organisms. Despite its ecological importance, historic and future global changes in stratification phenology are unknown. Here, we used a lake-climate model ensemble and long-term observational data, to investigate changes in lake stratification phenology across the Northern Hemisphere from 1901 to 2099. Under the high-greenhouse-gas-emission scenario, stratification will begin 22.0 ± 7.0 days earlier and end 11.3 ± 4.7 days later by the end of this century. It is very likely that this 33.3 ± 11.7 day prolongation in stratification will accelerate lake deoxygenation with subsequent effects on nutrient mineralization and phosphorus release from lake sediments. Further misalignment of lifecycle events, with possible irreversible changes for lake ecosystems, is also likely.
U2 - 10.1038/s41467-021-22657-4
DO - 10.1038/s41467-021-22657-4
M3 - Article
VL - 12
JO - Nature Communications
JF - Nature Communications
SN - 2041-1723
M1 - 2318 (2021)
ER -