Thomas G Huntington, Ph.D. (Former Employee)
Science and Products
Filter Total Items: 94
Historical changes in lake ice-out dates as indicators of climate change in New England, 1850-2000 Historical changes in lake ice-out dates as indicators of climate change in New England, 1850-2000
No abstract available.
Authors
Glenn A. Hodgkins, Ivan C. James, Thomas G. Huntington
Historical trend in ice thickness on the Piscataquis river, near Dover-Foxcroft, central Maine Historical trend in ice thickness on the Piscataquis river, near Dover-Foxcroft, central Maine
No abstract available.
Authors
Thomas G. Huntington, Glenn A. Hodgkins, Robert W. Dudley
Assessment of calcium status in Maine forests: Review and future projection Assessment of calcium status in Maine forests: Review and future projection
Forest harvesting and acidic deposition can cause substantial decreases in the calcium (Ca) inventory of forest soils if such losses are not replenished through mineral weathering, atmospheric deposition, or fertilization. The net balance between losses and gains defines the forest Ca status. Site-specific studies have measured Ca pools and fluxes in Maine forests, but no synthesis has...
Authors
T.G. Huntington
Changes in the number and timing of days of ice-affected flow on northern New England rivers, 1930-2000 Changes in the number and timing of days of ice-affected flow on northern New England rivers, 1930-2000
Historical dates of ice-affected flows for 16 rural, unregulated rivers in northern New England, USA were analyzed. The total annual days of ice-affected flow decreased significantly (p 0.1) over the 20th century at 12 of the 16 rivers. On average, for the nine longest-record rivers, the total annual days of ice-affected flow decreased by 20 days from 1936 to 2000, with most of the...
Authors
G.A. Hodgkins, R. W. Dudley, T.G. Huntington
Summer low flows in New England during the 20th Century Summer low flows in New England during the 20th Century
High springtime river flows came earlier by one to two weeks in large parts of northern New England during the 20th Century. In this study it was hypothesized that late spring/early summer recessional flows and late summer/early fall low flows could also be occurring earlier. This could result in a longer period of low flow recession and a decrease in the magnitude of low flows. To test...
Authors
Glenn A. Hodgkins, R. W. Dudley, Thomas G. Huntington
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
Filter Total Items: 94
Historical changes in lake ice-out dates as indicators of climate change in New England, 1850-2000 Historical changes in lake ice-out dates as indicators of climate change in New England, 1850-2000
No abstract available.
Authors
Glenn A. Hodgkins, Ivan C. James, Thomas G. Huntington
Historical trend in ice thickness on the Piscataquis river, near Dover-Foxcroft, central Maine Historical trend in ice thickness on the Piscataquis river, near Dover-Foxcroft, central Maine
No abstract available.
Authors
Thomas G. Huntington, Glenn A. Hodgkins, Robert W. Dudley
Assessment of calcium status in Maine forests: Review and future projection Assessment of calcium status in Maine forests: Review and future projection
Forest harvesting and acidic deposition can cause substantial decreases in the calcium (Ca) inventory of forest soils if such losses are not replenished through mineral weathering, atmospheric deposition, or fertilization. The net balance between losses and gains defines the forest Ca status. Site-specific studies have measured Ca pools and fluxes in Maine forests, but no synthesis has...
Authors
T.G. Huntington
Changes in the number and timing of days of ice-affected flow on northern New England rivers, 1930-2000 Changes in the number and timing of days of ice-affected flow on northern New England rivers, 1930-2000
Historical dates of ice-affected flows for 16 rural, unregulated rivers in northern New England, USA were analyzed. The total annual days of ice-affected flow decreased significantly (p 0.1) over the 20th century at 12 of the 16 rivers. On average, for the nine longest-record rivers, the total annual days of ice-affected flow decreased by 20 days from 1936 to 2000, with most of the...
Authors
G.A. Hodgkins, R. W. Dudley, T.G. Huntington
Summer low flows in New England during the 20th Century Summer low flows in New England during the 20th Century
High springtime river flows came earlier by one to two weeks in large parts of northern New England during the 20th Century. In this study it was hypothesized that late spring/early summer recessional flows and late summer/early fall low flows could also be occurring earlier. This could result in a longer period of low flow recession and a decrease in the magnitude of low flows. To test...
Authors
Glenn A. Hodgkins, R. W. Dudley, Thomas G. Huntington
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.