C
C. R. Beel
Researcher at Queen's University
Publications - 11
Citations - 158
C. R. Beel is an academic researcher from Queen's University. The author has contributed to research in topics: Permafrost & Arctic. The author has an hindex of 6, co-authored 10 publications receiving 109 citations. Previous affiliations of C. R. Beel include Purdue University & University of Otago.
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Journal ArticleDOI
Constraints on the late Quaternary glacial history of the Inylchek and Sary-Dzaz valleys from in situ cosmogenic 10Be and 26Al, eastern Kyrgyz Tian Shan
Nathaniel A. Lifton,C. R. Beel,Clas Hättestrand,Christine Kassab,Irina Rogozhina,Richard V. Heermance,Michael E. Oskin,Douglas W. Burbank,Robin Blomdin,Robin Blomdin,Natacha Gribenski,Marc W. Caffee,Brent M. Goehring,Jakob Heyman,M. Ivanov,Yanan Li,Yingkui Li,Dmitry Petrakov,Ryskul Usubaliev,Alexandru T. Codilean,Yixin Chen,Jon Harbor,Jon Harbor,Arjen P. Stroeven +23 more
TL;DR: The authors investigated the chronology of past glaciation in the Inylchek and Sary-Dzaz valleys in the eastern Kyrgyz Tian Shan, a tectonically active area with some of the highest peaks in the world outside of the Himalayas.
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Emerging dominance of summer rainfall driving High Arctic terrestrial-aquatic connectivity
C. R. Beel,J.K. Heslop,John F. Orwin,John F. Orwin,M. A. Pope,A. J. Schevers,J. K. Y. Hung,Melissa J. Lafrenière,Scott F. Lamoureux +8 more
TL;DR: In this paper, the authors integrated decade-long hydrometeorological and biogeochemical data from the High Arctic to show that shifts in the timing and magnitude of annual discharge patterns and stream power budgets are causing Arctic material transfer regimes to undergo fundamental changes.
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Quaternary evolution and ice sheet history of contrasting landscapes in Uummannaq and Sukkertoppen, western Greenland
TL;DR: In this paper, the authors analyzed in situ cosmogenic 10Be and 26Al in 26 rock samples from two high-elevation landscapes adjacent to the GIS, in Uummannaq and Sukkertoppen, western Greenland.
Journal ArticleDOI
Differential impact of thermal and physical permafrost disturbances on High Arctic dissolved and particulate fluvial fluxes.
C. R. Beel,Scott F. Lamoureux,John F. Orwin,John F. Orwin,M. A. Pope,Melissa J. Lafrenière,N. A. Scott +6 more
TL;DR: The transition from a nival-dominated fluvial regime to a regime where rainfall runoff is proportionately more important will be a likely tipping point to accelerated High Arctic change is concluded.
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Controls on slope-to-channel fine sediment connectivity in a largely ice-free valley, Hoophorn Stream, Southern Alps, New Zealand
TL;DR: In this paper, fine sediment mobilization on a slope segment hydrologically connected to a stream in the largely ice-free 8·3 km2 Hoophorn Valley, New Zealand, was monitored.