Simon J. Cook

ORCID: 0000-0003-1532-6532
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About
Contact & Profiles
Research Areas
  • Cryospheric studies and observations
  • Climate change and permafrost
  • Landslides and related hazards
  • Geology and Paleoclimatology Research
  • Winter Sports Injuries and Performance
  • Polar Research and Ecology
  • Arctic and Antarctic ice dynamics
  • Flood Risk Assessment and Management
  • Hydrology and Watershed Management Studies
  • Methane Hydrates and Related Phenomena
  • Species Distribution and Climate Change
  • Ecology and Vegetation Dynamics Studies
  • Microbial Community Ecology and Physiology
  • Climate Change Communication and Perception
  • Plant and animal studies
  • Environmental Education and Sustainability
  • Geochemistry and Geologic Mapping
  • Hydrology and Sediment Transport Processes
  • Disaster Management and Resilience
  • Wildlife Ecology and Conservation
  • Icing and De-icing Technologies
  • Scientific Research and Discoveries
  • Environmental and Cultural Studies in Latin America and Beyond
  • Atmospheric and Environmental Gas Dynamics
  • Risk Perception and Management

University of Dundee
2017-2025

Aberystwyth University
2008-2024

Planetary Science Institute
2024

British Geological Survey
2021

University of Minnesota
2021

United States Geological Survey
2021

University of Nottingham
2021

Schlumberger (British Virgin Islands)
2020

Manchester Metropolitan University
2013-2016

V. B. Sochava Institute of Geography
2010-2011

Abstract. Supraglacial, moraine-dammed and ice-dammed lakes represent a potential glacial lake outburst flood (GLOF) threat to downstream communities in many mountain regions. This has motivated the development of empirical relationships predict volume given measurement surface area obtained from satellite imagery. Such are based on notion that depth, scale predictably. We critically evaluate performance these existing by examining global database depths, areas volumes. Results show depth...

10.5194/esurf-3-559-2015 article EN cc-by Earth Surface Dynamics 2015-12-14

Abstract Many Karakoram glaciers periodically undergo surges during which large volumes of ice and debris are rapidly transported downglacier, usually at a rate 1–2 orders magnitude greater than quiescence. Here we identify eight recent in the region map their surface velocities using cross‐correlation feature tracking on optical satellite imagery. In total, present 44 velocity data sets, show that generally short‐lived, lasting between 3 5 years most cases, have rapid buildup relaxation...

10.1002/2015jf003515 article EN Journal of Geophysical Research Earth Surface 2015-06-19

Abstract. Glaciers of the Bolivian Andes represent an important water resource for Andean cities and mountain communities, yet relatively little work has assessed changes in their extent over recent decades. In many regions, glacier recession been accompanied by development proglacial lakes, which can pose a glacial lake outburst flood (GLOF) hazard. However, no studies have such lakes Bolivia despite GLOF incidents here. Our mapping from satellite imagery reveals overall areal shrinkage...

10.5194/tc-10-2399-2016 article EN cc-by ˜The œcryosphere 2016-10-20

Abstract Glaciers are highly effective agents of erosion that have profoundly shaped Earth’s surface, but there is uncertainty about how glacial should be parameterised in landscape evolution models. Glacial rate usually modelled as a function glacier sliding velocity, the empirical basis for this relationship weak. In turn, climate assumed to control velocity and hence erosion, too lacks scrutiny. Here, we present statistically robust relationships between rates, velocities, from global...

10.1038/s41467-020-14583-8 article EN cc-by Nature Communications 2020-02-06

Himalayan glaciers are undergoing rapid mass loss but rates of contemporary change lack long-term (centennial-scale) context. Here, we reconstruct the extent and surfaces 14,798 during Little Ice Age (LIA), 400 to 700 years ago. We show that they have lost at least 40 % their LIA area between 390 586 km3 ice; 0.92 1.38 mm Sea Level Equivalent. The rate ice since has been - 0.011 0.020 m w.e./year, which is an order magnitude lower than reported in literature. Rates depend on monsoon...

10.1038/s41598-021-03805-8 article EN cc-by Scientific Reports 2021-12-20

Abstract. Glacial lake outburst floods (GLOFs) are among the most concerning consequences of retreating glaciers in mountain ranges worldwide. GLOFs have attracted significant attention amongst scientists and practitioners past 2 decades, with particular interest physical drivers mechanisms GLOF hazard socioeconomic other human-related developments that affect vulnerabilities to events. This increased research focus on is reflected gradually increasing number papers published annually. study...

10.5194/nhess-22-3041-2022 article EN cc-by Natural hazards and earth system sciences 2022-09-19

Assessing the extent to which glacial lake outburst floods (GLOFs) are increasing in frequency modern times and whether their incidence is driven by anthropogenic climate change requires historical context. However, progress on this issue hampered incomplete GLOF inventories, especially remote mountain regions. Here, we exploit high-resolution, multi-temporal satellite aerial imagery, documentary data identify events across glacierized Cordilleras of Peru Bolivia, using a set diagnostic...

10.1016/j.gloplacha.2021.103722 article EN cc-by Global and Planetary Change 2021-12-18

Abstract Size is a fundamental property of landslides, but it described inconsistently within the scientific literature. There currently no widely adopted size classification system applicable to all landslide types. A Scopus database search shows most used descriptor term large , refer landslides with volumes spanning ten orders magnitude. Some descriptors are unintuitive or potentially misleading (e.g. massive which describes material property). We argue that formal scheme would encourage...

10.1007/s10346-023-02131-6 article EN cc-by Landslides 2023-09-29

Abstract As the world’s glaciers recede in response to a warming atmosphere, change magnitude and frequency of related hazards is expected. Among most destructive are glacier lake outburst floods (GLOFs), their future evolution concerning for local populations sustainable development policy. Central this better understanding triggers. There long‐standing assumption that earthquakes major GLOF trigger, seismic activity consistently included as key hazard assessment criterion. Here, we provide...

10.1029/2023gl105578 article EN cc-by Geophysical Research Letters 2024-03-30

Glacier bed overdeepenings are ubiquitous in glacier systems and likely exert significant influence on ice dynamics, subglacial hydrology, stability. Understanding of overdeepening formation evolution has been hampered by an absence quantitative empirical studies their distribution morphology, with process insights having drawn largely from theoretical or numerical studies. To address this shortcoming, we first map the potential beneath Antarctic Greenland sheets using a GIS-based algorithm...

10.1016/j.quascirev.2016.07.012 article EN cc-by-nc-nd Quaternary Science Reviews 2016-07-21

The Bolivian Andes have experienced sustained and widespread glacier mass loss in recent decades. Glacier recession has been accompanied by the development of proglacial lakes, which pose a glacial lake outburst flood (GLOF) risk to downstream communities infrastructure. Previous research identified three potentially dangerous lakes Andes, but no attempt yet made model GLOF inundation from these lakes. We generated 2-m resolution DEMs stereo tri-stereo SPOT 6/7 satellite images drive...

10.1007/s11069-018-3486-6 article EN cc-by Natural Hazards 2018-09-26

Abstract Climate change has implications for water resources by increasing temperature, shifting precipitation patterns and altering the timing of snowfall glacier melt, leading to shifts in seasonality river flows. Here, Soil & Water Assessment Tool was run using downscaled temperature projections from five global climate models (GCMs) their multi-model mean estimate potential impact on balance components sub-basins Upper Indus Basin (UIB) under two emission (RCP4.5 RCP8.5) future...

10.2166/wcc.2021.233 article EN cc-by Journal of Water and Climate Change 2021-11-29

Continuity of sediment transfer through glacial systems is essential to maintain subglacial bedrock erosion, yet at temperate glaciers with overdeepened beds, where fluvial transport should be greatly limited by adverse slopes, remains poorly understood. Complex multiple processes in has been indicated the presence large frontal moraine systems, supraglacial debris mixed origin, thick basal ice sequences, and englacial thrusts eskers. At Svínafellsjökull, comprising decimetre-thick...

10.1016/j.quascirev.2017.11.027 article EN cc-by-nc-nd Quaternary Science Reviews 2017-12-15

Glacial landsystems in the high-Arctic have been reported to undergo geomorphological transformation during deglaciation. This research evaluates moraine evolution over a decadal timescale at Midtre Lovénbreen, Svalbard. work is of interest because glacial landforms developed Svalbard used as an analogue for Pleistocene mid-latitude glaciation. Ground penetrating radar was investigate subsurface characteristics moraines. To determine surface change, LiDAR topographic data set (obtained 2003)...

10.1016/j.geomorph.2018.03.027 article EN cc-by-nc-nd Geomorphology 2018-03-29

Glacier retreat in northern latitudes exposes new landscapes that may develop soils and ecosystems, which turn sequester carbon serve as a negative climate change feedback. Proglacial soil development landscape evolution were investigated using transects from three high-latitude glacial systems (Tarfala, Sweden; Vatnajökull, Iceland; Zackenberg, Greenland). Soil samples analysed for organic (OC) concentration, bacteriohopanepolyol biomarkers (BHPs, membrane lipids trace major microbial...

10.1016/j.scitotenv.2025.178723 article EN cc-by The Science of The Total Environment 2025-03-01

10.1038/s41558-025-02275-4 article EN Nature Climate Change 2025-03-21

Abstract. Glacierised Peruvian mountain ranges are experiencing accelerated, climate-change-driven glacier ice loss. Peru's second highest range, the Cordillera Huayhuash, has lost about 40 % (∼ 34 km2) of its cover since 1970s. Newly exposed landscapes prone to a number hazard processes including formation and evolution glacial lakes, changing stability conditions slopes, rapid mass movements. In this study, we integrate analysis meteorological data, remotely sensed images field...

10.5194/nhess-25-1207-2025 article EN cc-by Natural hazards and earth system sciences 2025-03-28
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