Cottonwood Management at Theodore Roosevelt National Park, North Dakota
July 6, 2017
This data release consists of the following components:
Sex ratio data from cottonwood trees at random points on the floodplain in the North and South units of Theodore Roosevelt National Park, ND. These data were used to investigate the effects of age, height above, and distance from the channel on mortality of male and female trees of plains cottonwood (Populus deltoides subsp. monilifera) as described in the Friedman and Griffin (2017) report.
Tree core and tree ring data from the North and South Units of Theodore Roosevelt National Park, North Dakota. South Unit data was collected in April 2012, North Unit data was collected in the summer and fall of 2010. The trees are located on the floodplain of the Little Missouri River in Theodore Roosevelt National Park. These data were used to reconstruct flow and climate as described in the Friedman and Griffin (2017) report and in other documents cited by that report. The tree ring data is presented in Standard Tucson format.
Floodplain and riparian cottonwood forest areas in the South Unit were digitized as separate shapefiles using 2010 NAIP imagery. They were mapped to assist management of cottonwood forests by increasing understanding of the relation between geomorphic setting, flow, precipitation, temperature, and other factors.
Edges of water, channel centerline, valley bottom centerline, extent of valley bottom, and estimated bankfull channel data for the Little Missouri River in the North and South Units were mapped as separate shapefiles from 2010 NAIP imagery as well.
Sex ratio data from cottonwood trees at random points on the floodplain in the North and South units of Theodore Roosevelt National Park, ND. These data were used to investigate the effects of age, height above, and distance from the channel on mortality of male and female trees of plains cottonwood (Populus deltoides subsp. monilifera) as described in the Friedman and Griffin (2017) report.
Tree core and tree ring data from the North and South Units of Theodore Roosevelt National Park, North Dakota. South Unit data was collected in April 2012, North Unit data was collected in the summer and fall of 2010. The trees are located on the floodplain of the Little Missouri River in Theodore Roosevelt National Park. These data were used to reconstruct flow and climate as described in the Friedman and Griffin (2017) report and in other documents cited by that report. The tree ring data is presented in Standard Tucson format.
Floodplain and riparian cottonwood forest areas in the South Unit were digitized as separate shapefiles using 2010 NAIP imagery. They were mapped to assist management of cottonwood forests by increasing understanding of the relation between geomorphic setting, flow, precipitation, temperature, and other factors.
Edges of water, channel centerline, valley bottom centerline, extent of valley bottom, and estimated bankfull channel data for the Little Missouri River in the North and South Units were mapped as separate shapefiles from 2010 NAIP imagery as well.
Citation Information
Publication Year | 2017 |
---|---|
Title | Cottonwood Management at Theodore Roosevelt National Park, North Dakota |
DOI | 10.5066/F7Z60M9V |
Authors | Jonathan M Friedman, Eleanor R. Griffin |
Product Type | Data Release |
Record Source | USGS Asset Identifier Service (AIS) |
USGS Organization | Fort Collins Science Center |
Rights | This work is marked with CC0 1.0 Universal |
Related
Management of plains cottonwood at Theodore Roosevelt National Park, North Dakota
Establishment of cottonwood trees is driven by flood-induced channel migration, which provides the new surfaces necessary for successful germination and survival. Along the Little Missouri River the largest floods typically result from snowmelt in March or April. Seed release occurs in early summer, and seedlings usually germinate in moist, open locations on point bars at relatively low...
Authors
Jonathan M. Friedman, Eleanor R. Griffin
Related
Management of plains cottonwood at Theodore Roosevelt National Park, North Dakota
Establishment of cottonwood trees is driven by flood-induced channel migration, which provides the new surfaces necessary for successful germination and survival. Along the Little Missouri River the largest floods typically result from snowmelt in March or April. Seed release occurs in early summer, and seedlings usually germinate in moist, open locations on point bars at relatively low...
Authors
Jonathan M. Friedman, Eleanor R. Griffin