Thermokarst Lakes as a Source of Atmospheric CH4 During the Last Deglaciation (2007)
Walter, K.M., Edwards, M.E., Grosse, G., Zimov, S.A., Chapin III, F.S.
Polar ice-core records suggest that an arctic or boreal source was responsible for more than 30% of the large increase in global atmospheric methane (CH4) concentration during deglacial climate...
Thermokarst Lakes as a Source of Atmospheric CH4 During the Last Deglaciation (2007)
Walter, K.M, Edwards, M. E, Grosse, G, Zimov, S. A, Chapin III, F. S.
Polar ice-core records suggest that an arctic or boreal source was responsible for more than 30% of the large increase in global atmospheric methane (CH4) concentration during deglacial climate...
Thermokarst lakes as a source of atmospheric CH4 during the last deglaciation (2007)
Walter, K.M., Edwards, M.E., Grosse, G., Zimov, S.A., Chapin, F.S. III
Polar ice-core records suggest that an arctic or boreal source was responsible for more than 30% of the large increase in global atmospheric methane (CH4) concentration during deglacial climate...
Wooller, M.J., Zazula, G.D., Edwards, M.E., Froese, D.G., Boone, R.D., Parker, C., ...
The nature of vegetation cover present in Beringia during the last glaciation remains unclear. Uncertainty rests partly with the limitations of conventional paleoecological methods. A lack of...
Wooller, M.J, Zazula, G.D, Edwards, M.E, Froese, D.G, Boone, R.D, Parker, C., ...
The nature of vegetation cover present in Beringia during the last glaciation remains unclear. Uncertainty rests partly with the limitations of conventional paleoecological methods. A lack of...
Last Interglacial Arctic warmth confirms polar amplification of climate change (2006)
Anderson, P., Bermike, O., Bigelow, N., Brigham-Grette, J., Duvall, M., Edwards, M.E., ...
The warmest millennia of at least the past 250,000 years occurred during the Last Interglaciation, when global ice volumes were similar to or smaller than today and systematic variations in Earth’s...
Last Interglacial Arctic warmth confirms polar amplification of climate change (2006)
Anderson, P., Bermike, O., Bigelow, N., Brigham-Grette, J., Duvall, M., Edwards, M.E., ...
The warmest millennia of at least the past 250,000 years occurred during the Last Interglaciation, when global ice volumes were similar to or smaller than today and systematic variations in Earth’s...
Conserving Idealized Landscapes: Past History, Public Perception and Future Management (2006)
The New Forest is one of the most visited regions of Britain. It has recently been designated a National Park in recognition of its unique wood pasture ecosystems, a traditional land-use system, its...
Conserving Idealized Landscapes: Past History, Public Perception and Future Management (2006)
The New Forest is one of the most visited regions of Britain. It has recently been designated a National Park in recognition of its unique wood pasture ecosystems, a traditional land-use system, its...
Rae, D.A., Armbruster, W.S., Edwards, M.E., Svengård-Barre, M.
We assessed the effects of both biotic processes and abiotic factors on the community composition of vascular plant species and invertebrates at a site in northern Norway. Plant species were assigned...
Rae, D.A, Armbruster, W.S, Edwards, M.E, Svengård-Barre, M
We assessed the effects of both biotic processes and abiotic factors on the community composition of vascular plant species and invertebrates at a site in northern Norway. Plant species were assigned...
Simulating arctic climate warmth and icefield retreat in the last interglaciation (2006)
Otto-Bliesner, Beth L., Marsha, Shawn J., Overpeck, Jonathan T., Miller, Gifford H., Hu, Aixue X., Edwards, M.E
In the future, Arctic warming and the melting of polar glaciers will be considerable, but the magnitude of both is uncertain. We used a global climate model, a dynamic ice sheet model, and...
Simulating arctic climate warmth and icefield retreat in the last interglaciation (2006)
Otto-Bliesner, Beth L., Marsha, Shawn J., Overpeck, Jonathan T., Miller, Gifford H., Hu, Aixue X., Edwards, M.E
In the future, Arctic warming and the melting of polar glaciers will be considerable, but the magnitude of both is uncertain. We used a global climate model, a dynamic ice sheet model, and...
Bigelow, N. H., Brubaker, L. B., Edwards, M. E., Harrison, Sandy P., Prentice, I. Colin, Anderson, P. M., ...
Kaplan, Jed O., Bigelow, N. H., Prentice, I. Colin, Harrison, Sandy P., Bartlein, Patrick J., Christensen, T. R., ...
Bigelow, N. H., Brubaker, L. B., Edwards, M. E., Harrison, S. P., Prentice, I. C., Anderson, P. M., ...
A unified scheme to assign pollen samples to vegetation types was used to reconstruct vegetation patterns north of 55°N at the last glacial maximum (LGM) and mid-Holocene (6000 years B.P.). The...
Kaplan, J. O., Bigelow, N. H., Prentice, I. C., Harrison, S. P., Bartlein, P. J., Christensen, T. R., ...
Large variations in the composition, structure, and function of Arctic ecosystems are determined by climatic gradients, especially of growing-season warmth, soil moisture, and snow cover. A unified...
Kaplan, J. O., Bigelow, N. H., Prentice, I. C., Harrison, S.P., Bartlein, P.J., Christensen, T.R., ...
Large variations in the composition, structure, and function of Arctic ecosystems are determined by climatic gradients, especially of growing-season warmth, soil moisture, and snow cover. A unified...
Kaplan, J. O, Bigelow, N. H, Prentice, I. C, Harrison, S. P, Bartlein, P. J, Christensen, T. R, ...
Large variations in the composition, structure, and function of Arctic ecosystems are determined by climatic gradients, especially of growing-season warmth, soil moisture, and snow cover. A unified...
Holocene paleoclimate data from the Arctic: testing models of global climate change (2001)
To evaluate the spatial variability ofArctic climate change during the present interglacial, CAPE Project Members compiled well-dated terrestrial, marine, and ice-core paleoenvironmental records...
Holocene paleoclimate data from the Arctic: testing models of global climate change (2001)
To evaluate the spatial variability ofArctic climate change during the present interglacial, CAPE Project Members compiled well-dated terrestrial, marine, and ice-core paleoenvironmental records...
A 45 m outcrop of Quaternary sediments on Birch Creek, near Circle, Alaska, reveals a record of #uctuating environmental conditions that probably spans several glacial}interglacial cycles. From base...
A 45 m outcrop of Quaternary sediments on Birch Creek, near Circle, Alaska, reveals a record of #uctuating environmental conditions that probably spans several glacial}interglacial cycles. From base...
Wildfire responses to abrupt climate change in North America
Marlon, J. R., Bartlein, P. J., Walsh, M. K., Harrison, S. P., Brown, K. J., Edwards, M. E., ...
It is widely accepted, based on data from the last few decades and on model simulations, that anthropogenic climate change will cause increased fire activity. However, less attention has been paid to...