2001
DOI: 10.1016/s0034-4257(00)00162-0
|View full text |Cite
|
Sign up to set email alerts
|

The Influence of Vegetation Index and Spatial Resolution on a Two-Date Remote Sensing-Derived Relation to C4 Species Coverage

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1
1
1

Citation Types

0
45
0

Year Published

2005
2005
2022
2022

Publication Types

Select...
6
2

Relationship

0
8

Authors

Journals

citations
Cited by 67 publications
(45 citation statements)
references
References 36 publications
0
45
0
Order By: Relevance
“…Each region may be deemed a mosaic, where vegetation types are found at scales ranging from 100 m to 1 km, while microsite variations (e.g., changes in relief due to hummocks and frost action in tussock tundra) may occur within centimetres to metres (McFadden et al, 1998). Second, small-scale vegetation studies may be ideal, but the harsh Arctic climate and the remote nature of field sites do not always render such studies feasible Jacobsen and Hansen, 1999), nor are they necessarily useful in extrapolating to broader expanses of land (Dungan, 1998;Lobo et al, 1998;Ostendorf and Reynolds, 1998;Davidson and Csillag, 2001). Remote sensing provides the potential to characterize surface variables that control carbon fluxes over landscapes (i.e., 100 m 2 to 100 km 2 ) or regions (i.e., > 100 km 2 ) (Hope et al, 1995).…”
Section: Introductionmentioning
confidence: 99%
“…Each region may be deemed a mosaic, where vegetation types are found at scales ranging from 100 m to 1 km, while microsite variations (e.g., changes in relief due to hummocks and frost action in tussock tundra) may occur within centimetres to metres (McFadden et al, 1998). Second, small-scale vegetation studies may be ideal, but the harsh Arctic climate and the remote nature of field sites do not always render such studies feasible Jacobsen and Hansen, 1999), nor are they necessarily useful in extrapolating to broader expanses of land (Dungan, 1998;Lobo et al, 1998;Ostendorf and Reynolds, 1998;Davidson and Csillag, 2001). Remote sensing provides the potential to characterize surface variables that control carbon fluxes over landscapes (i.e., 100 m 2 to 100 km 2 ) or regions (i.e., > 100 km 2 ) (Hope et al, 1995).…”
Section: Introductionmentioning
confidence: 99%
“…Field investigations are usually limited to short-term, plot scale studies that lack both the temporal and spatial coverage needed to characterize grass dynamics directly in a comprehensive manner. Recently, this data deficit has been addressed through remote sensing methods to quantify grass cover in space and time [16,46,47]. Observations from satellite data, in fact, motivated the present analysis and are used to characterize vegetation cover for the regional-scale land surface hydrological model presented herein.…”
Section: Introductionmentioning
confidence: 99%
“…Depending on the objective and scale of the research, both ground-based radiometers and satellite imagery have been widely utilized within grassland research to estimate plant biophysical parameters such as ALB (Davidson and Csillag 2001;Flombaum and Sala 2007). Typically, ALB is estimated by establishing an empirical relationship between the destructively measured biomass and the transformations of 2 or more remotely sensed spectral bands.…”
Section: Alb Estimationmentioning
confidence: 99%