N. H. Bigelow

Publication List Details

Period

2002 - 9999

Number

13

Co-Authors

Holocene Loess and Paleosols in Central Alaska: A Proxy Record of Holocene Climate Change, (9999)

Bigelow, N. H., Beget, J. E.

Episodic Holocene loess deposition and soil formation in the sediments of the Nenana valley of Central Alaska may reflect Holocene climate change. Periods of loess deposition seem to correlate with...

Interglacial extension of the boreal forest limit in the Noatak Valley, Northwest Alaska: evidence from an exhumed river-cut bluff and debris apron (2004)

Edwards, M.E., Hamilton, T.D., Elias, S.E., Bigelow, N.H., Krumhardt, A.P.

Numerous exposures of Pleistocene sediments occur in the Noatak basin, which extends for 130 km along the Noatak River in northwestern Alaska. Nk-37, an extensive bluff exposure near the west end of...

Climate change and Arctic ecosystems: 2. Modelling, palaeodata-model comparisons, and future projections (2003)

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...

Climate change and Arctic ecosystems: 1. Vegetation changes north of 55°N between the last glacial maximum, mid-Holocene, and present (2003)

Bigelow, N.H., Brubaker, Linda B., Edwards, M.E., Harrison, S.P., Prentice, I. Colin, 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...

Climate change and Arctic ecosystems: 1. Vegetation changes north of 55 degrees N between the last glacial maximum, mid-Holocene, and present (2003)

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...

Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections (2003)

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...

Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections (2003)

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...

Climate change and Arctic ecosystems: 2. Modeling, paleodata-model comparisons, and future projections (2003)

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...

Geographic and temporal variations in fire history in boreal ecosystems of Alaska (2002)

Lynch, J.A., Clark, J.S., Bigelow, N.H., Edwards, M.E., Finney, B.P.

Charcoal and pollen analyses were used to determine geographic and temporal patterns of fire importance in boreal forests of the Kenai Peninsula and interior Alaska. Sieved, large charcoal particles...