Skip to main content

ETHNOS_APP

Home • Search • Journals • List 0

Torben R Christensen

Biographic Data

ID5970159
NAMETorben R Christensen
GIVEN NAMESTorben R
FAMILY NAMEChristensen
SIGNATURECHRISTENSEN T R
AFFILIATIONSLund University
ORCID0000-0002-4917-148X
VERIFIEDYes
TOTAL WORKS46
TOTAL CITATIONS115
WORKS AS AUTHOR46
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1991
LATEST PUBLICATION YEAR2021
H-INDEX7
  • Climatic Factors Influencing the Anthrax Outbreak of 2016 in Siberia, Russia

    Open Access•Ekaterina Ezhova, Dmitry Orlov et al.•ARTICLE•EcoHealth•2021

    In 2016, an outbreak of anthrax killing thousands of reindeer and affecting dozens of humans occurred on the Yamal peninsula, Northwest Siberia, after 70 years of epidemiological situation without outbreaks. The trigger of the outbreak has been ascribed to the activation of spores due to permafrost thaw that was accelerated during the summer heat wave. The focus of our study is on the dynamics of local environmental factors in connection with the…

  • The missing pieces for better future predictions in subarctic ecosystems

    Open Access•Yinan He, Didac Pascual et al.•ARTICLE•AMBIO•2021•References: 70

    Arctic and subarctic ecosystems are experiencing substantial changes in hydrology, vegetation, permafrost conditions, and carbon cycling, in response to climatic change and other anthropogenic drivers, and these changes are likely to continue over this century. The total magnitude of these changes results from multiple interactions among these drivers. Field measurements can address the overall responses to different changing drivers, but are les…

  • Multi-year data-model evaluation reveals the importance of nutrient availability over climate in arctic ecosystem C dynamics

    Open Access•Efrén López–Blanco, M Jackowicz-Korczyński et al.•ARTICLE•Environmental Research Letters•2020

    Arctic tundra is a globally important store for carbon (C). However, there is a lack of reference sites characterising C exchange dynamics across annual cycles. Based on the Greenland Ecosystem Monitoring (GEM) programme, here we present 9–11 years of flux and ecosystem data across the period 2008–2018 from two wetland sites in Greenland: Zackenberg (74°N) and Kobbefjord (64°N). The Zackenberg fen was a strong C sink despite its higher latitude a…

  • Key indicators of Arctic climate change

    Open Access•Jason E Box, William Colgan et al.•ARTICLE•Environmental Research Letters•2019

    Key observational indicators of climate change in the Arctic, most spanning a 47 year period demonstrate fundamental changes among nine key elements of the Arctic system. We find that, coherent with increasing air temperature, there is an intensification of the hydrological cycle, evident from increases in humidity, precipitation, river discharge, glacier equilibrium line altitude and land ice wastage. Downward trends continue in sea ice thicknes…

  • Potential future methane emission hot spots in Greenland

    Open Access•Marilena Geng, Jens Hesselbjerg Christensen et al.•ARTICLE•Environmental Research Letters•2018

    Climate models have been making significant progress encompassing an increasing number of complex feedback mechanisms from natural ecosystems. Permafrost thaw and subsequent induced greenhouse gas emissions, however, remain a challenge for climate models at large. Deducing permafrost conditions and associated greenhouse gas emissions from parameters that are simulated in climate models would be a helpful step towards estimating emission budgets f…

  • Postscript

    Open Access•Torben R Christensen, Elmer Topp-Jørgensen et al.•ARTICLE•AMBIO•2017•References: 1

    As documented with examples in this special issue of Ambio, the Greenland Ecosystem Monitoring (GEM) Programme in its first 20 years has focused on both detailed and very comprehensive studies of specific ecosystems in order to monitor and understand ecosystem patterns and processes. An international review of GEM conducted in 2015 praised the programme for its comprehensiveness, but also saw an untapped potential for a wider use of GEM data and …

  • A synthesis of the arctic terrestrial and marine carbon cycles under pressure from a dwindling cryosphere

    Open Access•Frans-Jan W Parmentier, Frans‐Jan W Parmentier et al.•ARTICLE•AMBIO•2017•References: 126

    The current downturn of the arctic cryosphere, such as the strong loss of sea ice, melting of ice sheets and glaciers, and permafrost thaw, affects the marine and terrestrial carbon cycles in numerous interconnected ways. Nonetheless, processes in the ocean and on land have been too often considered in isolation while it has become increasingly clear that the two environments are strongly connected: Sea ice decline is one of the main causes of th…

  • Toward a statistical description of methane emissions from arctic wetlands

    Open Access•Norbert Pirk, Mikhail Mastepanov et al.•ARTICLE•AMBIO•2017•Cited by: 1•References: 42

    Methane (CH 4 ) emissions from arctic tundra typically follow relations with soil temperature and water table depth, but these process-based descriptions can be difficult to apply to areas where no measurements exist. We formulated a description of the broader temporal flux pattern in the growing season based on two distinct CH 4 source components from slow and fast-turnover carbon. We used automatic closed chamber flux measurements from NE Green…

  • Focus on the impact of climate change on wetland ecosystems and carbon dynamics

    Open Access•Lei Meng, Nigel T Roulet et al.•ARTICLE•Environmental Research Letters•2016

    The renewed growth in atmospheric methane (CH4) since 2007 after a decade of stabilization has drawn much attention to its causes and future trends. Wetlands are the single largest source of atmospheric CH4. Understanding wetland ecosystems and carbon dynamics is critical to the estimation of global CH4 and carbon budgets. After approximately 7 years of CH4 related research following the renewed growth in atmospheric CH4, Environmental Research L…

  • Biomass offsets little or none of permafrost carbon release from soils, streams, and wildfire

    Open Access•Benjamin W Abbott, Jeremy B Jones et al.•ARTICLE•Environmental Research Letters•2016

    As the permafrost region warms, its large organic carbon pool will be increasingly vulnerable to decomposition, combustion, and hydrologic export. Models predict that some portion of this release will be offset by increased production of Arctic and boreal biomass; however, the lack of robust estimates of net carbon balance increases the risk of further overshooting international emissions targets. Precise empirical or model-based assessments of t…

  • Large herbivore grazing affects the vegetation structure and greenhouse gas balance in a high arctic mire

    Open Access•Julie Maria Falk, Niels M Schmidt et al.•ARTICLE•Environmental Research Letters•2015

    Herbivory is an important part of most ecosystems and affects the ecosystems' carbon balance both directly and indirectly. Little is known about herbivory and its impact on the carbon balance in high arctic mire ecosystems. We hypothesized that trampling and grazing by large herbivores influences the vegetation density and composition and thereby also the carbon balance. In 2010, we established fenced exclosures in high arctic Greenland to preven…

  • Rescuing Valuable Arctic Vegetation Data for Biodiversity Models, Ecosystem Models and a Panarctic Vegetation Classification

    Open Access•Donald A Walker, Inger G Alsos et al.•ARTICLE•ARCTIC•2013

    TEST 02 - Elsevier's Scopus, the largest abstract and citation database of peer-reviewed literature. Search and access research from the science, technology, medicine, social sciences and arts and humanities fields

  • Rapid responses of permafrost and vegetation to experimentally increased snow cover in sub-arctic Sweden

    Open Access•Margareta Johansson, Terry V Callaghan et al.•ARTICLE•Environmental Research Letters•2013

    Increased snow depth already observed, and that predicted for the future are of critical importance to many geophysical and biological processes as well as human activities. The future characteristics of sub-arctic landscapes where permafrost is particularly vulnerable will depend on complex interactions between snow cover, vegetation and permafrost. An experimental manipulation was, therefore, set up on a lowland peat plateau with permafrost, in…

  • Effects of drought conditions on the carbon dioxide dynamics in a temperate peatland

    Open Access•Magnus Lund, Torben R Christensen et al.•ARTICLE•Environmental Research Letters•2012

    Drought is arguably the most important regulator of inter-annual variation in net ecosystem CO exchange (NEE) in peatlands. This study investigates effects of drought periods on NEE and its components, gross primary production (GPP) and ecosystem respiration (R), on the basis of eddy covariance measurements of land-atmosphere exchange of CO in 2006-2009 in a south Swedish nutrient-poor peatland. Two drought periods had dissimilar effects on the C…

  • Monitoring the Multi-Year Carbon Balance of a Subarctic Palsa Mire with Micrometeorological Techniques

    Open Access•Torben R Christensen, M Jackowicz-Korczyński et al.•ARTICLE•AMBIO•2012•Cited by: 2•References: 34

  • The Man, the Myth, the Legend

    Open Access•Margareta Johansson, Christer Jonasson et al.•ARTICLE•AMBIO•2012•Cited by: 2•References: 13

  • Post Scriptum

    Open Access•Torben R Christensen, Margareta Johansson et al.•ARTICLE•AMBIO•2012

  • Environmental Monitoring and Research in the Abisko Area—An Overview

    Open Access•Christer Jonasson, Mats Sonesson et al.•ARTICLE•AMBIO•2012•Cited by: 3•References: 63

  • Multiple Effects of Changes in Arctic Snow Cover

    Open Access•Terry V Callaghan, Margareta Johansson et al.•ARTICLE•AMBIO•2011•Cited by: 7•References: 76

  • Multi-Decadal Changes in Tundra Environments and Ecosystems

    Open Access•Terry V Callaghan, C E Tweedie et al.•ARTICLE•AMBIO•2011•Cited by: 6•References: 63

  • Plant and Vegetation Dynamics on Disko Island, West Greenland

    Open Access•Terry V Callaghan, Torben R Christensen et al.•ARTICLE•AMBIO•2011•Cited by: 5•References: 39

  • Past and Present Permafrost Temperatures in the Abisko Area

    Open Access•Margareta Johansson, Jonas Akerman et al.•ARTICLE•AMBIO•2011•Cited by: 2•References: 17

  • The carbon budget of the northern cryosphere region

    Open Access•A D McGuire, Robie W Macdonald et al.•ARTICLE•Current Opinion in Environmental…•2010•Cited by: 1

  • Ecological Dynamics Across the Arctic Associated with Recent Climate Change

    Open Access•Eric Post, Mads C Forchhammer et al.•ARTICLE•Science•2009

    Assessing the Arctic The Arctic is experiencing some of the most rapid climate change currently under way across the globe, but consequent ecological responses have not been widely reported. At the close of the Fourth International Polar Year, Post et al. (p. 1355 ) review observations on ecological impacts in this sensitive region. The widespread changes occurring in terrestrial, freshwater, and marine systems, presage changes at lower latitudes…

  • What Determines the Current Presence or Absence of Permafrost in the Torneträsk Region, a Sub-arctic Landscape in Northern Sweden

    Margareta Johansson, Torben R Christensen et al.•ARTICLE•AMBIO•2006•Cited by: 4•References: 29

    In a warming climate, permafrost is likely to be significantly reduced and eventually disappear from the sub-Arctic region. This will affect people at a range of scales, from locally by slumping of buildings and roads, to globally as melting of permafrost will most likely increase the emissions of the powerful greenhouse gas methane, which will further enhance global warming. In order to predict future changes in permafrost, it is crucial to unde…

Next
  • Biodiversity, Distributions and Adaptations of Arctic Species in the Context of Environmental Change

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 19

    The individual of a species is the basic unit which responds to climate and UV-B changes, and it responds over a wide range of time scales. The diversity of animal, plant and microbial species appears to be low in the Arctic, and decreases from the boreal forests to the polar deserts of the extreme North but primitive species are particularly abundant. This latitudinal decline is associated with an increase in super-dominant species that occupy a…

  • Effects of Changes in Climate on Landscape and Regional Processes, and Feedbacks to the Climate System

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 12

    Biological and physical processes in the Arctic system operate at various temporal and spatial scales to impact large-scale feedbacks and interactions with the earth system. There are four main potential feedback mechanisms between the impacts of climate change on the Arctic and the global climate system: albedo, greenhouse gas emissions or uptake by ecosystems, greenhouse gas emissions from methane hydrates, and increased freshwater fluxes that …

  • Effects on the Function of Arctic Ecosystems in the Short- and Long-term Perspectives

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 11

    Historically, the function of Arctic ecosystems in terms of cycles of nutrients and carbon has led to low levels of primary production and exchanges of energy, water and greenhouse gases have led to low local and regional cooling. Sequestration of carbon from atmospheric CO2, in extensive, cold organic soils and the high albedo from low, snow-covered vegetation have had impacts on regional climate. However, many aspects of the functioning of Arct…

  • Effects on the Structure of Arctic Ecosystems in the Short- and Long-term Perspectives

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 9

    Historically, the function of Arctic ecosystems in terms of cycles of nutrients and carbon has led to low levels of primary production and exchanges of energy, water and greenhouse gases have led to low local and regional cooling. Sequestration of carbon from atmospheric CO2, in extensive, cold organic soils and the high albedo from low, snow-covered vegetation have had impacts on regional climate. However, many aspects of the functioning of Arct…

  • Multiple Effects of Changes in Arctic Snow Cover

    Open Access•Terry V Callaghan, Margareta Johansson et al.•ARTICLE•AMBIO•2011•Cited by: 7•References: 76

  • Rationale, Concepts and Approach to the Assessment

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 7

  • Responses to Projected Changes in Climate and UV-B at the Species Level

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 7

    Environmental manipulation experiments showed that species respond individualistically to each environmental-change variable. The greatest responses of plants were generally to nutrient, particularly nitrogen, addition. Summer warming experiments showed that woody plant responses were dominant and that mosses and lichens became less abundant. Responses to warming were controlled by moisture availability and snow cover. Many invertebrates increase…

  • Multi-Decadal Changes in Tundra Environments and Ecosystems

    Open Access•Terry V Callaghan, C E Tweedie et al.•ARTICLE•AMBIO•2011•Cited by: 6•References: 63

  • Past Changes in Arctic Terrestrial Ecosystems, Climate and UV Radiation

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 6

    At the last glacial maximum, vast ice sheets covered many continental areas. The beds of some shallow seas were exposed thereby connecting previously separated landmasses. Although some areas were ice-free and supported a flora and fauna, mean annual temperatures were 10-13 degrees C colder than during the Holocene. Within a few millennia of the glacial maximum, deglaciation started, characterized by a series of climatic fluctuations between abou…

  • Plant and Vegetation Dynamics on Disko Island, West Greenland

    Open Access•Terry V Callaghan, Torben R Christensen et al.•ARTICLE•AMBIO•2011•Cited by: 5•References: 39

  • Synthesis of Effects in Four Arctic Subregions

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 5

    An assessment of impacts on Arctic terrestrial ecosystems has emphasized geographical variability in responses of species and ecosystems to environmental change. This variability is usually associated with north-south gradients in climate, biodiversity, vegetation zones, and ecosystem structure and function. It is clear, however, that significant east-west variability in environment, ecosystem structure and function, environmental history, and re…

  • What Determines the Current Presence or Absence of Permafrost in the Torneträsk Region, a Sub-arctic Landscape in Northern Sweden

    Margareta Johansson, Torben R Christensen et al.•ARTICLE•AMBIO•2006•Cited by: 4•References: 29

    In a warming climate, permafrost is likely to be significantly reduced and eventually disappear from the sub-Arctic region. This will affect people at a range of scales, from locally by slumping of buildings and roads, to globally as melting of permafrost will most likely increase the emissions of the powerful greenhouse gas methane, which will further enhance global warming. In order to predict future changes in permafrost, it is crucial to unde…

  • Uncertainties and Recommendations

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 4

    An assessment of the impacts of changes in climate and UV-B radiation on Arctic terrestrial ecosystems, made within the Arctic Climate Impacts Assessment (ACIA), highlighted the profound implications of projected warming in particular for future ecosystem services, biodiversity and feedbacks to climate. However, although our current understanding of ecological processes and changes driven by climate and UV-B is strong in some geographical areas a…

  • Environmental Monitoring and Research in the Abisko Area—An Overview

    Open Access•Christer Jonasson, Mats Sonesson et al.•ARTICLE•AMBIO•2012•Cited by: 3•References: 63

  • Monitoring the Multi-Year Carbon Balance of a Subarctic Palsa Mire with Micrometeorological Techniques

    Open Access•Torben R Christensen, M Jackowicz-Korczyński et al.•ARTICLE•AMBIO•2012•Cited by: 2•References: 34

  • The Man, the Myth, the Legend

    Open Access•Margareta Johansson, Christer Jonasson et al.•ARTICLE•AMBIO•2012•Cited by: 2•References: 13

  • Past and Present Permafrost Temperatures in the Abisko Area

    Open Access•Margareta Johansson, Jonas Akerman et al.•ARTICLE•AMBIO•2011•Cited by: 2•References: 17

  • Toward a statistical description of methane emissions from arctic wetlands

    Open Access•Norbert Pirk, Mikhail Mastepanov et al.•ARTICLE•AMBIO•2017•Cited by: 1•References: 42

    Methane (CH 4 ) emissions from arctic tundra typically follow relations with soil temperature and water table depth, but these process-based descriptions can be difficult to apply to areas where no measurements exist. We formulated a description of the broader temporal flux pattern in the growing season based on two distinct CH 4 source components from slow and fast-turnover carbon. We used automatic closed chamber flux measurements from NE Green…

  • The carbon budget of the northern cryosphere region

    Open Access•A D McGuire, Robie W Macdonald et al.•ARTICLE•Current Opinion in Environmental…•2010•Cited by: 1

  • Key Findings and Extended Summaries

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 1

    TEST 02 - Elsevier's Scopus, the largest abstract and citation database of peer-reviewed literature. Search and access research from the science, technology, medicine, social sciences and arts and humanities fields

  • Greenland wants tourism

    Open Access•Torben Christensen, Torben R Christensen•ARTICLE•Polar Record•1992•Cited by: 1

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Arctic and sub-Arctic soil emissions

    Open Access•Torben Christensen, Torben R Christensen•ARTICLE•Polar Record•1991•References: 22

    Climate models predict a substantial warming at high latitudes following the enhanced greenhouse effect caused by anthropogenic emissions of carbon dioxide (CO 2 ), methane (CH 4 ), and various other trace gases. Arctic and sub-Arctic soils contain large amounts of organic carbon that could be made increasingly available for decomposition in a wanner climate due to deepening of the biologically-active layer and increased thermokarst erosion. This…

  • Greenland wants tourism

    Open Access•Torben Christensen, Torben R Christensen•ARTICLE•Polar Record•1992•Cited by: 1

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Report from the First Annual Conference of the National Institute for Global Environmental Change

    Open Access•Torben Christensen, Torben R Christensen•ARTICLE•Polar Record•1992

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Uncertainties and Recommendations

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 4

    An assessment of the impacts of changes in climate and UV-B radiation on Arctic terrestrial ecosystems, made within the Arctic Climate Impacts Assessment (ACIA), highlighted the profound implications of projected warming in particular for future ecosystem services, biodiversity and feedbacks to climate. However, although our current understanding of ecological processes and changes driven by climate and UV-B is strong in some geographical areas a…

  • Past Changes in Arctic Terrestrial Ecosystems, Climate and UV Radiation

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 64

    At the last glacial maximum, vast ice sheets covered many continental areas. The beds of some shallow seas were exposed thereby connecting previously separated landmasses. Although some areas were ice-free and supported a flora and fauna, mean annual temperatures were 10–13°C colder than during the Holocene. Within a few millennia of the glacial maximum, deglaciation started, characterized by a series of climatic fluctuations between about 18 000…

  • Rationale, Concepts and Approach to the Assessment

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 7

  • Uncertainties and Recommendations

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 20

    An assessment of the impacts of changes in climate and UV-B radiation on Arctic terrestrial ecosystems, made within the Arctic Climate Impacts Assessment (ACIA), highlighted the profound implications of projected warming in particular for future ecosystem services, biodiversity and feedbacks to climate. However, although our current understanding of ecological processes and changes driven by climate and UV-B is strong in some geographical areas a…

  • Synthesis of Effects in Four Arctic Subregions

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 5

    An assessment of impacts on Arctic terrestrial ecosystems has emphasized geographical variability in responses of species and ecosystems to environmental change. This variability is usually associated with north-south gradients in climate, biodiversity, vegetation zones, and ecosystem structure and function. It is clear, however, that significant east-west variability in environment, ecosystem structure and function, environmental history, and re…

  • Responses to Projected Changes in Climate and UV-B at the Species Level

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 149

    Environmental manipulation experiments showed that species respond individualistically to each environmental-change variable. The greatest responses of plants were generally to nutrient, particularly nitrogen, addition. Summer warming experiments showed that woody plant responses were dominant and that mosses and lichens became less abundant. Responses to warming were controlled by moisture availability and snow cover. Many invertebrates increase…

  • Effects on the Structure of Arctic Ecosystems in the Short- and Long-term Perspectives

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 9

    Historically, the function of Arctic ecosystems in terms of cycles of nutrients and carbon has led to low levels of primary production and exchanges of energy, water and greenhouse gases have led to low local and regional cooling. Sequestration of carbon from atmospheric CO2, in extensive, cold organic soils and the high albedo from low, snow-covered vegetation have had impacts on regional climate. However, many aspects of the functioning of Arct…

  • Responses to Projected Changes in Climate and UV-B at the Species Level

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 7

    Environmental manipulation experiments showed that species respond individualistically to each environmental-change variable. The greatest responses of plants were generally to nutrient, particularly nitrogen, addition. Summer warming experiments showed that woody plant responses were dominant and that mosses and lichens became less abundant. Responses to warming were controlled by moisture availability and snow cover. Many invertebrates increase…

  • Past Changes in Arctic Terrestrial Ecosystems, Climate and UV Radiation

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 6

    At the last glacial maximum, vast ice sheets covered many continental areas. The beds of some shallow seas were exposed thereby connecting previously separated landmasses. Although some areas were ice-free and supported a flora and fauna, mean annual temperatures were 10-13 degrees C colder than during the Holocene. Within a few millennia of the glacial maximum, deglaciation started, characterized by a series of climatic fluctuations between abou…

  • Key Findings and Extended Summaries

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 9

  • Effects of Changes in Climate on Landscape and Regional Processes, and Feedbacks to the Climate System

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 88

    Biological and physical processes in the Arctic system operate at various temporal and spatial scales to impact large-scale feedbacks and interactions with the earth system. There are four main potential feedback mechanisms between the impacts of climate change on the Arctic and the global climate system: albedo, greenhouse gas emissions or uptake by ecosystems, greenhouse gas emissions from methane hydrates, and increased freshwater fluxes that …

  • Rationale, Concepts and Approach to the Assessment

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 27

    A general recognition that the Arctic will amplify global climate warming, that UV-B radiation may continue to increase there because of possible delays in the repair of stratospheric ozone, and that the Arctic environment and its peoples are likely to be particularly susceptible to such environmental changes stimulated an international assessment of climate change impacts. The Arctic Climate Impacts Assessment (ACIA) is a four-year study, culmin…

  • Effects on the Structure of Arctic Ecosystems in the Short- and Long-term Perspectives

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 110

    Species individualistic responses to warming and increased UV-B radiation are moderated by the responses of neighbors within communities, and trophic interactions within ecosystems. All of these responses lead to changes in ecosystem structure. Experimental manipulation of environmental factors expected to change at high latitudes showed that summer warming of tundra vegetation has generally led to smaller changes than fertilizer addition. Some o…

  • Effects of Changes in Climate on Landscape and Regional Processes, and Feedbacks to the Climate System

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 12

    Biological and physical processes in the Arctic system operate at various temporal and spatial scales to impact large-scale feedbacks and interactions with the earth system. There are four main potential feedback mechanisms between the impacts of climate change on the Arctic and the global climate system: albedo, greenhouse gas emissions or uptake by ecosystems, greenhouse gas emissions from methane hydrates, and increased freshwater fluxes that …

  • Biodiversity, Distributions and Adaptations of Arctic Species in the Context of Environmental Change

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 19

    The individual of a species is the basic unit which responds to climate and UV-B changes, and it responds over a wide range of time scales. The diversity of animal, plant and microbial species appears to be low in the Arctic, and decreases from the boreal forests to the polar deserts of the extreme North but primitive species are particularly abundant. This latitudinal decline is associated with an increase in super-dominant species that occupy a…

  • Key Findings and Extended Summaries

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 1

    TEST 02 - Elsevier's Scopus, the largest abstract and citation database of peer-reviewed literature. Search and access research from the science, technology, medicine, social sciences and arts and humanities fields

  • Effects on the Function of Arctic Ecosystems in the Short- and Long-term Perspectives

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•Cited by: 11

    Historically, the function of Arctic ecosystems in terms of cycles of nutrients and carbon has led to low levels of primary production and exchanges of energy, water and greenhouse gases have led to low local and regional cooling. Sequestration of carbon from atmospheric CO2, in extensive, cold organic soils and the high albedo from low, snow-covered vegetation have had impacts on regional climate. However, many aspects of the functioning of Arct…

  • Synthesis of Effects in Four Arctic Subregions

    Terry V Callaghan, Lars Olof Björn et al.•ARTICLE•AMBIO•2004•References: 12

    An assessment of impacts on Arctic terrestrial ecosystems has emphasized geographical variability in responses of species and ecosystems to environmental change. This variability is usually associated with north-south gradients in climate, biodiversity, vegetation zones, and ecosystem structure and function. It is clear, however, that significant east-west variability in environment, ecosystem structure and function, environmental history, and re…

  • What Determines the Current Presence or Absence of Permafrost in the Torneträsk Region, a Sub-arctic Landscape in Northern Sweden

    Margareta Johansson, Torben R Christensen et al.•ARTICLE•AMBIO•2006•Cited by: 4•References: 29

    In a warming climate, permafrost is likely to be significantly reduced and eventually disappear from the sub-Arctic region. This will affect people at a range of scales, from locally by slumping of buildings and roads, to globally as melting of permafrost will most likely increase the emissions of the powerful greenhouse gas methane, which will further enhance global warming. In order to predict future changes in permafrost, it is crucial to unde…

  • Ecological Dynamics Across the Arctic Associated with Recent Climate Change

    Open Access•Eric Post, Mads C Forchhammer et al.•ARTICLE•Science•2009

    Assessing the Arctic The Arctic is experiencing some of the most rapid climate change currently under way across the globe, but consequent ecological responses have not been widely reported. At the close of the Fourth International Polar Year, Post et al. (p. 1355 ) review observations on ecological impacts in this sensitive region. The widespread changes occurring in terrestrial, freshwater, and marine systems, presage changes at lower latitudes…

  • The carbon budget of the northern cryosphere region

    Open Access•A D McGuire, Robie W Macdonald et al.•ARTICLE•Current Opinion in Environmental…•2010•Cited by: 1

  • Multiple Effects of Changes in Arctic Snow Cover

    Open Access•Terry V Callaghan, Margareta Johansson et al.•ARTICLE•AMBIO•2011•Cited by: 7•References: 76

Environmental Science (38 works) · Climate change and permafrost (34 works) · Arctic (30 works) · Geography (26 works) · Ecology (25 works) · Ecology (24 works) · Climate change (22 works) · Ecosystem (21 works) · Geology (21 works) · Biology (18 works)

Ethnos_APP • Open Source Project • MIT License • Frontend v2.0.0 • Privacy and Cookies • API Documentation: api.ethnos.app/docs • API Source Code: GitHub • DOI: 10.5281/zenodo.17049435 • Frontend Source Code: GitHub • DOI: 10.5281/zenodo.17050053 • cruz.rio.br • Expectantes Misericordiae