Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America

Despite their generally isolated geographic locations, the freshwaters of the north are subjected to a wide spectrum of environmental stressors. High-latitude regions are especially sensitive to the effects of recent climatic warming, which have already resulted in marked regime shifts in the biolog...

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Main Authors: David W. Schindler, John P. Smol
Format: Text
Language:English
Published: Royal Swedish Academy of Sciences 2006
Subjects:
Ice
Online Access:https://doi.org/10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2
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spelling ftbioone:10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2 2023-07-30T04:01:10+02:00 Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America David W. Schindler John P. Smol David W. Schindler John P. Smol world 2006-06-01 text/HTML https://doi.org/10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2 en eng Royal Swedish Academy of Sciences doi:10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2 All rights reserved. https://doi.org/10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2 Text 2006 ftbioone https://doi.org/10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2 2023-07-09T09:33:29Z Despite their generally isolated geographic locations, the freshwaters of the north are subjected to a wide spectrum of environmental stressors. High-latitude regions are especially sensitive to the effects of recent climatic warming, which have already resulted in marked regime shifts in the biological communities of many Arctic lakes and ponds. Important drivers of these limnological changes have included changes in the amount and duration of snow and ice cover, and, for rivers and lakes in their deltas, the frequency and extent of spring floods. Other important climate-related shifts include alterations in evaporation and precipitation ratios, marked changes in the quality and quantity of lake and river water inflows due to accelerated glacier and permafrost melting, and declining percentages of precipitation that falls as snow. The depletion of stratospheric ozone over the north, together with the clarity of many Arctic lakes, renders them especially susceptible to damage from ultraviolet radiation. In addition, the long-range atmospheric transport of pollutants, coupled with the focusing effects of contaminant transport from biological vectors to some local ecosystems (e.g., salmon nursery lakes, ponds draining seabird colonies) and biomagnification in long food chains, have led to elevated concentrations of many persistent organic pollutants (e.g., insecticides, which have never been used in Arctic regions) and other pollutants (e.g., mercury). Rapid development of gas and oil pipelines, mining for diamonds and metals, increases in human populations, and the development of all-season roads, seaports, and hydroelectric dams will stress northern aquatic ecosystems. The cumulative effects of these stresses will be far more serious than those caused by changing climate alone. Text Arctic Ice permafrost Subarctic BioOne Online Journals Arctic
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language English
description Despite their generally isolated geographic locations, the freshwaters of the north are subjected to a wide spectrum of environmental stressors. High-latitude regions are especially sensitive to the effects of recent climatic warming, which have already resulted in marked regime shifts in the biological communities of many Arctic lakes and ponds. Important drivers of these limnological changes have included changes in the amount and duration of snow and ice cover, and, for rivers and lakes in their deltas, the frequency and extent of spring floods. Other important climate-related shifts include alterations in evaporation and precipitation ratios, marked changes in the quality and quantity of lake and river water inflows due to accelerated glacier and permafrost melting, and declining percentages of precipitation that falls as snow. The depletion of stratospheric ozone over the north, together with the clarity of many Arctic lakes, renders them especially susceptible to damage from ultraviolet radiation. In addition, the long-range atmospheric transport of pollutants, coupled with the focusing effects of contaminant transport from biological vectors to some local ecosystems (e.g., salmon nursery lakes, ponds draining seabird colonies) and biomagnification in long food chains, have led to elevated concentrations of many persistent organic pollutants (e.g., insecticides, which have never been used in Arctic regions) and other pollutants (e.g., mercury). Rapid development of gas and oil pipelines, mining for diamonds and metals, increases in human populations, and the development of all-season roads, seaports, and hydroelectric dams will stress northern aquatic ecosystems. The cumulative effects of these stresses will be far more serious than those caused by changing climate alone.
author2 David W. Schindler
John P. Smol
format Text
author David W. Schindler
John P. Smol
spellingShingle David W. Schindler
John P. Smol
Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America
author_facet David W. Schindler
John P. Smol
author_sort David W. Schindler
title Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America
title_short Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America
title_full Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America
title_fullStr Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America
title_full_unstemmed Cumulative Effects of Climate Warming and Other Human Activities on Freshwaters of Arctic and Subarctic North America
title_sort cumulative effects of climate warming and other human activities on freshwaters of arctic and subarctic north america
publisher Royal Swedish Academy of Sciences
publishDate 2006
url https://doi.org/10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2
op_coverage world
geographic Arctic
geographic_facet Arctic
genre Arctic
Ice
permafrost
Subarctic
genre_facet Arctic
Ice
permafrost
Subarctic
op_source https://doi.org/10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2
op_relation doi:10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2
op_rights All rights reserved.
op_doi https://doi.org/10.1579/0044-7447(2006)35[160:CEOCWA]2.0.CO;2
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