Richard Iestyn Woolway

Richard Iestyn Woolway

Top Cited Scholar 2026
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Richard Iestyn Woolway

School of Ocean Sciences, Bangor University

Research Focus & Metrics

Academic Career Length

13Years (2014-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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14 July 2020 in Nature Reviews Earth & Environment
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RWR. Iestyn Woolway
R. Iestyn Woolway
BKBenjamin Kraemer
Benjamin Kraemer
JLJohn D. Lenters
John D. Lenters
CMChristopher Merchant
Christopher Merchant
COCatherine M. O’rEilly
Catherine M. O’rEilly
SSSapna Sharma
Sapna Sharma

2 June 2021 in Nature
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Journal Article
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SJStephen F. Jane
Stephen F. Jane
GHGretchen J. A. Hansen
Gretchen J. A. Hansen
BKBenjamin Kraemer
Benjamin Kraemer
PLPeter R. Leavitt
Peter R. Leavitt
JMJoshua L. Mincer
Joshua L. Mincer
KRKevin Rose
Kevin Rose

18 March 2019 in Nature Geoscience
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Journal Article
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RWR. Iestyn Woolway
R. Iestyn Woolway
CMChristopher Merchant
Christopher Merchant

20 January 2021 in Nature
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Journal Article
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RWR. Iestyn Woolway
R. Iestyn Woolway
Eleanor JenningsEleanor Jennings
Eleanor Jennings
TSTom Shatwell
Tom Shatwell
MGMalgorzata Golub
Malgorzata Golub
Donald C. PiersonDonald C. Pierson
Donald C. Pierson
SMStephen Christopher Maberly
Stephen Christopher Maberly

19 April 2021 in Nature Communications
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Journal Article
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RWR. Iestyn Woolway
R. Iestyn Woolway
SSSapna Sharma
Sapna Sharma
GWGesa A. Weyhenmeyer
Gesa A. Weyhenmeyer
ADAndrey Debolskiy
Andrey Debolskiy
MGMalgorzata Golub
Malgorzata Golub
Eleanor JenningsEleanor Jennings
Eleanor Jennings
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.

18 July 2022 in BioScience
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Journal Article
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RWR Iestyn Woolway
R Iestyn Woolway
SSSapna Sharma
Sapna Sharma
JSJohn P Smol
John P Smol
Our planet is being subjected to unprecedented climate change, with far-reaching social and ecological repercussions. Below the waterline, aquatic ecosystems are being affected by multiple climate-related and anthropogenic stressors, the combined effects of which are poorly understood and rarely appreciated at the global stage. A striking consequence of climate change on aquatic ecosystems is that many are experiencing shorter periods of ice cover, as well as earlier and longer summer stratified seasons, which often result in a cascade of ecological and environmental consequences, such as warmer summer water temperatures, alterations in lake mixing and water levels, declines in dissolved oxygen, increased likelihood of cyanobacterial algal blooms, and the loss of habitat for native cold-water fisheries. The repercussions of a changing climate include impacts on freshwater supplies, water quality, biodiversity, and the ecosystem benefits that they provide to society.