The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska

Geomorphic and hydraulic complexity within five streams representing 200 years of stream development were examined in Glacier Bay National Park, Alaska. Channel geomorphic units (CGUs) were mapped using a hierarchical approach, which defined stream habitat according to morphological and hydraulic ch...

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Published in:River Research and Applications
Main Authors: Klaar, Megan, Maddock, Ian, Milner, A.M.
Format: Article in Journal/Newspaper
Language:unknown
Published: John Wiley & Sons 2009
Subjects:
Online Access:http://eprints.worc.ac.uk/577/
http://www3.interscience.wiley.com/journal/121673908/abstract
https://doi.org/10.1002/rra.1235
id ftunivworcester:oai:wrap.eprints.org:577
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spelling ftunivworcester:oai:wrap.eprints.org:577 2023-05-15T16:20:28+02:00 The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska Klaar, Megan Maddock, Ian Milner, A.M. 2009-02-04 http://eprints.worc.ac.uk/577/ http://www3.interscience.wiley.com/journal/121673908/abstract https://doi.org/10.1002/rra.1235 unknown John Wiley & Sons Klaar, Megan, Maddock, Ian orcid:0000-0001-5072-8700 and Milner, A.M. (2009) The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska. River Research and Applications. ISSN 1535-1467 doi:10.1002/rra.1235 G Geography (General) Q Science (General) GE Environmental Sciences GB Physical geography Article PeerReviewed 2009 ftunivworcester https://doi.org/10.1002/rra.1235 2022-03-02T19:57:14Z Geomorphic and hydraulic complexity within five streams representing 200 years of stream development were examined in Glacier Bay National Park, Alaska. Channel geomorphic units (CGUs) were mapped using a hierarchical approach, which defined stream habitat according to morphological and hydraulic characteristics. Detailed hydraulic assessment within the geomorphic units allowed differences in hydraulic characteristics across the 200-year chronosequence to be documented. Channel geomorphology and hydrology changed as stream age increased. Younger streams were dominated by fast flowing geomorphic units such as rapids and riffles with little hydraulic or landscape diversity. As stream age increased, slower flowing habitat units such as glides and pools became more dominant, resulting in increased geomorphic, hydraulic and landscape diversity. These results suggest that geomorphic and hydraulic complexity develop over time, creating habitat features likely to be favoured by instream biota, enhancing biodiversity and abundance. Article in Journal/Newspaper glacier Alaska University of Worcester: Worcester Research and Publications Glacier Bay River Research and Applications 25 10 1331 1338
institution Open Polar
collection University of Worcester: Worcester Research and Publications
op_collection_id ftunivworcester
language unknown
topic G Geography (General)
Q Science (General)
GE Environmental Sciences
GB Physical geography
spellingShingle G Geography (General)
Q Science (General)
GE Environmental Sciences
GB Physical geography
Klaar, Megan
Maddock, Ian
Milner, A.M.
The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska
topic_facet G Geography (General)
Q Science (General)
GE Environmental Sciences
GB Physical geography
description Geomorphic and hydraulic complexity within five streams representing 200 years of stream development were examined in Glacier Bay National Park, Alaska. Channel geomorphic units (CGUs) were mapped using a hierarchical approach, which defined stream habitat according to morphological and hydraulic characteristics. Detailed hydraulic assessment within the geomorphic units allowed differences in hydraulic characteristics across the 200-year chronosequence to be documented. Channel geomorphology and hydrology changed as stream age increased. Younger streams were dominated by fast flowing geomorphic units such as rapids and riffles with little hydraulic or landscape diversity. As stream age increased, slower flowing habitat units such as glides and pools became more dominant, resulting in increased geomorphic, hydraulic and landscape diversity. These results suggest that geomorphic and hydraulic complexity develop over time, creating habitat features likely to be favoured by instream biota, enhancing biodiversity and abundance.
format Article in Journal/Newspaper
author Klaar, Megan
Maddock, Ian
Milner, A.M.
author_facet Klaar, Megan
Maddock, Ian
Milner, A.M.
author_sort Klaar, Megan
title The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska
title_short The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska
title_full The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska
title_fullStr The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska
title_full_unstemmed The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska
title_sort development of hydraulic and geomorphic complexity in recently formed streams in glacier bay national park, alaska
publisher John Wiley & Sons
publishDate 2009
url http://eprints.worc.ac.uk/577/
http://www3.interscience.wiley.com/journal/121673908/abstract
https://doi.org/10.1002/rra.1235
geographic Glacier Bay
geographic_facet Glacier Bay
genre glacier
Alaska
genre_facet glacier
Alaska
op_relation Klaar, Megan, Maddock, Ian orcid:0000-0001-5072-8700 and Milner, A.M. (2009) The Development of Hydraulic and Geomorphic Complexity in Recently Formed Streams in Glacier Bay National Park, Alaska. River Research and Applications. ISSN 1535-1467
doi:10.1002/rra.1235
op_doi https://doi.org/10.1002/rra.1235
container_title River Research and Applications
container_volume 25
container_issue 10
container_start_page 1331
op_container_end_page 1338
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