Environ Monit Assess
DOI 10.1007/s10661-010-1768-x
Using digital time-lapse cameras to monitor
species-specific understorey and overstorey
phenology in support of wildlife habitat
assessment
Christopher W. Bater · Nicholas C. Coops ·
Michael A. Wulder · Thomas Hilker · Scott E. Nielsen ·
Greg McDermid · Gordon B. Stenhouse
Received: 6 July 2010 / Accepted: 21 October 2010
© The Author(s) 2010. This article is published with open access at Springerlink.com
Abstract Critical to habitat management is the
understanding of not only the location of animal food resources, but also the timing of their
availability. Grizzly bear (Ursus arctos) diets, for
example, shift seasonally as different vegetation
species enter key phenological phases. In this
paper, we describe the use of a network of seven
C. W. Bater (B) · N. C. Coops · T. Hilker
Department of Forest Resources Management,
University of British Columbia, 2424 Main Mall,
Vancouver, BC, V6T 1Z4, Canada
e-mail: cbater@interchange.ubc.ca
M. A. Wulder
Canadian Forest Service (Pacific Forestry Centre),
Natural Resources Canada, 506 West Burnside Road,
Victoria, BC, V8Z 1M5, Canada
S. E. Nielsen
Department of Renewable Resources,
University of Alberta, 751 General Services Building,
Edmonton, Alberta, T6G 2H1, Canada
G. McDermid
Department of Geography, University of Calgary,
2500 University Drive NW, Calgary, Alberta, T2N
1N4, Canada
G. B. Stenhouse
Foothills Research Institute, Hinton, Alberta,
T7V 1X6, Canada
ground-based digital camera systems to monitor understorey and overstorey vegetation within
species-specific regions of interest. Established
across an elevation gradient in western Alberta,
Canada, the cameras collected true-colour (RGB)
images daily from 13 April 2009 to 27 October
2009. Fourth-order polynomials were fit to an
RGB-derived index, which was then compared to
field-based observations of phenological phases.
Using linear regression to statistically relate the
camera and field data, results indicated that 61%
(r2 = 0.61, df = 1, F = 14.3, p = 0.0043) of the
variance observed in the field phenological phase
data is captured by the cameras for the start of
the growing season and 72% (r2 = 0.72, df = 1,
F = 23.09, p = 0.0009) of the variance in length
of growing season. Based on the linear regression
models, the mean absolute differences in residuals
between predicted and observed start of growing
season and length of growing season were 4 and
6 days, respectively. This work extends upon previous research by demonstrating that specific understorey and overstorey species can be targeted
for phenological monitoring in a forested environment, using readily available digital camera
technology and RGB-based vegetation indices.
Keywords Plant phenology ·
Near-surface remote sensing ·
Time-lapse photography · Ursus arctos
Environ Monit Assess
Introduction
Managing landscapes for grizzly bears (Ursus
arctos) is complicated given the diverse nature
of food resources and habitats used by bears
(McLellan and Hovey 2001; Hamer and Herrero
1987; Munro et al. 2006). The diet of grizzly bears
has been studied for over two decades in many
areas in North America and Europe, and is known
to comprise seasonally abundant, nutrient-rich
food (Hamer et al. 1991; Craighead et al. 1995;
Dahle et al. 1998; Persson et al. 2001; Nielsen et al.
2003; Munro et al. 2006). Generally, their diet is
highly diverse both temporally and spatially, as
is the case for most habitat generalists or omnivores. Individual bears may in fact travel large
distances to access high-quality food sources when
they become seasonally available (Rogers 1987).
In general, grizzly bear food habits and selection
patterns following den emergence in the spring
and prior to den entry in the fall may be divided
into three distinct seasons: hypophagia, early hyperphagia and late hyperphagia (Nielsen 2005).
During hypophagia, grizzly bears feed on roots of
Hedysarum spp. and occasionally carrion. During
early hyperphagia, their diet extends to ants, ungulate calves and green herbaceous material such
as cow-parsnip (Heracleum lanatum) and horsetail
(Equisetum spp.). During the later season, berries
such as buffalo berry (Shepherdia canadensis),
blueberry (Vaccinium myrtilloides) and huckleberry (Vaccinium membranaceum), as well as the
roots of Hedydarum spp., make up the majority
of their diet (Nielsen 2005). Munro et al. (2006)
grouped grizzly bear diet into nine major classes
which differed seasonally and among mountain
and foothills environments. Of the defined groups,
animal matter was most important from late May
to late June (most commonly moose, deer and
elk), with a wide variety of green vegetation,
including forbs and fruit, making up major components of their diet from late June through to
early October (Fig. 1). Thus, grizzly bears rely on
a variety of plant and animal species to satisfy
their nutritional requirements, with individuals
exhibiting seasonal shifts in diet and behaviour in
Fig. 1 Seasonal trends in digestible dry matter content of dominant vegetative food items found in grizzly bear feces
collected in west-central Alberta between 2001 and 2003 (drawn using data from Munro et al. (2006), Table 2)
Environ Monit Assess
response to changes in food availability (Munro
et al. 2006). As a result, the development of
spatially explicit food models operating at phenological scales matching those at which bears
perceive and select resources is a critical step
towards understanding their ecology (Nielsen
et al. 2003, 2010).
One possible approach to determine seasonality in plant communities is to assess changes
in the phenological stages through direct observation over multiple growing seasons and environmental conditions. While originally applied
to carbon-related studies of vegetation, previous
research indicates that changes in the timing of
plant developmental phases may signal important
inter-annual climatic variations (Reed et al. 1994;
White and Nemani 2003; Xiao and Moody 2004),
and may therefore be relevant to grizzly bear feeding patterns. Time series of phenology data can
be developed using single or multiple observers
at single locations, or through phenological networks, where multiple observers record observations of the same species at different locations
(Bertin 2008). At broad spatial scales, satellite
imagery, such as the normalized difference vegetation index, based on the normalized spectral
reflectance in the red and near infrared regions
of the electromagnetic spectrum, has been used
for documenting patterns of ‘leafing out’ in spring
(Botta et al. 2000; Studer et al. 2007). There are
limitations, however, related to the broad spatial
resolution of these sensors, which can be further
exacerbated by poor temporal resolution in areas
with persistent cloud cover. Other issues concerning satellite measurements are the need for adjustments due to changes in orbital and atmospheric
conditions, and possible influences of late snow
cover on the resultant data (Schwartz and Reed
1999; Studer et al. 2007).
The increasing popularity and use of inexpensive visible spectrum digital cameras in recent
years offers the potential to remotely monitor and
measure phenological events (Graham et al. 2006,
2010; Bradley et al. 2010). Repeat photography
allows sampling at very dense temporal resolutions, often at daily or hourly intervals, for
monitoring vegetation phenology. Mounting these
systems on towers or other platforms provides
data at an intermediate scale of observation, al-
lowing a contrast between field-based observations and satellite-derived measures (Richardson
et al. 2009). Close-range observation, often
referred to as near-surface remote sensing, facilitates the collection of high temporal and spatial
resolution data.
Many of the early applications of camera technology to phenological studies started in agriculture (Adamsen et al. 2000). For example, Purcell
(2000) utilised digital cameras to detect changes
in wheat and soybean canopies at a 1-m spatial
resolution over a growing season. Graham et al.
(2006) acquired daily images of mosses during
drying and moistening cycles to develop a comprehensive understanding of the changing status
of the species under different climatic conditions.
Richardson et al. (2007) recently mounted a commercially available digital web camera system on
a CO2 flux tower in Barlett, New Hampshire,
to observe deciduous vegetation green-up and to
make comparisons to changes in the fraction of
the photosynthetically active radiation absorbed
by the canopy. After initial success using data
obtained in 2006, a network of similar instruments
is being proposed to be installed on a larger
number of flux tower sites across North America,
and potentially as part of the National Ecological
Observation Network (described in Keller et al.
(2008)). Linking the phenological cycle through
these types of measurements to the drivers of
habitat and food availability for animal species
sensitive to phenological events has the potential
to be incorporated into wildlife habitat and nutritional landscape models (Nielsen et al. 2003,
2010) and provide further insight into the changing needs of animals. Grizzly bears in western
Alberta are particularly good candidates for a
study of this type, as an extensive body of knowledge related to their seasonal feeding habits and
home range usage exists.
In this paper, we demonstrate the potential
for imagery collected from a network of cameras
established across an elevation gradient in western
Alberta to be used to derive phenological patterns
of food species commonly used by grizzly bears.
We focus on 11 “regions of interest” within the
ground-based images delineating under- and overstorey species, many relevant to bear diets, to assess the capacity of the network to detect changes
Environ Monit Assess
in phenological phases and correlate these indicators with field observations.
Materials and methods
Study area
The eastern slopes of the Rocky Mountains in
Alberta, Canada, is a diverse region containing a mix of mature and young forest, wetlands
and alpine areas. A 90-km-long transect centred
near the town of Robb, Alberta (53.2215◦ N,
116.98392◦ W), was designed to capture a range
of phenological changes and growing seasons
attributes across known grizzly bear habitat. Six
sites were selected in pairs at three different elevation zones across the transect. One paired site
was placed within a coniferous dominated stand,
and the other paired site located in a more mixed
species site with between 20–40% deciduous trees.
Additionally, a seventh site was established in
a high-elevation coniferous stand, but no mixed
replicate could be found. Details on the sites, their
vegetation composition and location are summarized in Table 1.
Digital camera network setup
A detailed description of the phenological camera
network is provided in Bater et al. (Design and
installation of a camera network across an elevation gradient for habitat assessment. Instrumentation Science & Technology, submitted).
In summary, seven commercially available digital time-lapse camera systems manufactured by
Harbortronics (Fort Collins, Colorado, USA)
were installed (Table 2). The systems consist of a
Pentax digital single lens reflex camera slaved to
an intervalometer, which are sealed in a fiberglass
case. Power was provided by a solar panel and a
lithium ion battery. The cameras employ 23.5 ×
15.7 mm charged coupled device (CCD) sensors
with either 6.1 or 10.2 million effective pixels with
data recorded using a 4 GB SD memory card.
In each plot, a single camera was mounted 3 m
above the ground on a tall and dominant tree
and pointed north. To minimize directional effects
caused by solar movements, each camera was set
to record five JPEG images per day between 12:00
noon and 1:00 p.m. local time. Digital images were
archived as high-resolution JPEG images (2,000 ×
3,008 pixel or 2,592 × 3,872 pixel resolution with
Table 1 Summary of the camera sites, including forest cover type and coordinates
Site name
Easting (m)a
Northing (m)a
Forest type
Forest composition and
common names (basal area)
Elevation (m)b
Bryan spur
502,319
5,899,684
Mixed
1,093
Bryan spur
501,950
5,898,930
Coniferous
Fickle Lake
519,136
5,916,668
Mixed
Fickle Lake
518,537
5,916,058
Coniferous
Cadomin
5,877,276
Mixed
Cadomin
478,427
1,484
480,660
5,879,755
Coniferous
Prospect Creek
478,036
5,868,840
Coniferous
Lodgepole pine (16 m2 /ha),
trembling aspen (10 m2 /ha)
and spruce species (2 m2 /ha)
Open black spruce forest
(10 m2 /ha), bog
White spruce (22 m2 /ha),
trembling aspen (18 m2 /ha),
dead balsam poplar (4 m2 /ha),
closed forest
Riparian white spruce forest
(14 m2 /ha), bog
Riparian, balsam poplar (6 m2 /ha)
and white spruce (4 m2 /ha)
Open black spruce forest (6 m2 /ha),
occasional lodgepole pine, bog
High elevation, lodgepole
pine (20 m2 /ha)
a Projection:
b Ellipsoid:
1,092
970
951
1,458
1,714
Universal Transverse Mercator. Horizontal Datum: World Geodetic System 1984. Zone: 11 north
World Geodetic System 1984
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Table 2 Description of
the intervalometers and
cameras employed for the
phenology monitoring
program
Intervalometer
Model
Time of first daily capture
Number of captures
Interval between captures
Harbortronics Digisnap 2000
12:00 noon
5
12 min
Camera
Model
Pentax K100D or K200D digital
single lens reflex
23.5 × 15.7 mm CCD; 6.1 or
10.2 million effective pixels
18–55 mm, f 3.5–5.6
4 GB SD
High-quality JPEG
Sunlight
Program auto exposure (P)
200
Manual, set to infinity
18 mm
Disabled
Disabled
Sensor
Lens
Card
File type
White balance
Mode
ISO
Focus
Focal length
Shake reduction
Flash
three channels of 8-bit RGB data). Image file
ancillary data included date and time of acquisition. The cameras collected imagery for a single growing season in 2009, operating from 13
April (day of year = 103) to 27 October (day of
year = 300).
by Dierschke (1972) (Table 3). Codes for deciduous vegetation ranged from 0 indicating closed
bud, through to 6 (full leaf unfolding), to 10, which
represents dead vegetation. In the case of coniferous green vegetation, the codes ranged from 0
to 6, indicating closed bud (0) through to mature
shoots (6).
Field validation and phenophase codes
Image analysis
The seven camera locations were visited 12 times
throughout the growing season, and vegetation
were classified using phenophase codes developed
Table 3 Phenology codes developed by Dierschke (1972)
and recorded at monitoring sites for trees and shrubs
Vegetative (V)
Deciduous tree or shrub
0. Closed bud
1. Green leaf out but
not unfolded
2. Green leaf out, start
of unfolding
3. Leaf unfolding up to 25%
4. Leaf unfolding up to 50%
5. Leaf unfolding up to 75%
6. Full leaf unfolding
7. Stem/first leaves fading
8. Yellowing up to 50%
9. Yellowing over 50%
10. Dead
Conifer
0. Closed bud
1. Swollen bud
2. Split bud
3. Shoot capped
4. Shoot elongate
5. Shoot full length,
lighter green
6. Shoot mature,
equally green
Eleven homogenous under- and overstorey
species-specific regions of interest, observable
on the digital camera imagery, were selected
from the photos in order to assess vegetation
development at a high level of detail (Fig. 2,
Table 4). Using regions of interest or masks is a
commonly accepted method for analysing specific
portions of ground-based images. For example,
Ahrends et al. (2008) employed regions of interest
to isolate portions of individual ash and beech
crowns from a mixed canopy beneath a flux tower.
Ide and Oguma (2010) employed areas or regions
of interest to separate individual species where
image resolution and distance to target permitted.
Graham et al. (2010) segmented images into
deciduous, evergreen and understorey regions for
analysis.
The selection of an accurate vegetation index is required for automated image-based analyses of plant phenology. Previously, Woebbecke
et al. (1995) investigated five true-colour indices
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been used widely since (e.g. Meyer and Neto
2008). Recently, Richardson et al. (2007) developed a phenology monitoring program using a
digital RGB web camera, and employed a measure similar to the excess green index referred to
as 2G-RBi:
2G-RBi = 2µG − (µ R + µ B )
Fig. 2 Black and white example of a photo acquired at the
Bryan Spur mixed site, and size and positions of speciesspecific regions of interest which were analyzed
derived from digitized images to separate living plant material from soil and crop residue.
Woebbecke et al. (1995) determined that an excess green index was most effective, and it has
Table 4 Vegetation
species monitored within
image regions of interest
(1)
where µG , µ R and µ B are the camera observed
brightness values (raw DN) in the green, red
and blue channels, respectively. Richardson et al.
(2007) found good correlations between vegetation gross primary production as measured from
an eddy flux covariance tower. Thus, rather than
using a satellite-derived vegetation index, we employed the 2G-RBi index to monitor changes in
plant phenology within each species-specific region of interest (Fig. 2).
Many approaches have been developed to interpret phenological events from temporal variations in vegetation indices or, in this situation,
sequential digital imagery. Information on key
dates, such as the start and end of the growing season are possible (Waring et al. 2006).
One key method to extract these dates is based
on the seasonal-midpoint (or half-maximum) approach, which was designed to predict the initial leaf expansion of broadleaf forests (White
et al. 1999; Schwartz et al. 2002). The method
first calculates the annual minimum and maximum value for each pixel and the midpoint
is then calculated and added to the minimum.
This calculated value has the advantage over
other formulations in that it is sensitive to
site-specific variations in the range of values
Site
Region of interest species
Region of interest
species common name
Bryan Spur Mixed
Populus tremuloides
Vaccinium vitis-idaea
Vaccinium myrtilloides
Shepherdia canadensis
Populus tremuloides
Shepherdia canadensis
Equisetum arvense
Populus balsamifera
Shepherdia canadensis
Equisetum arvense, grass
Shepherdia canadensis
Trembling aspen
Lingon berry
Hillside blueberry
Buffalo berry
Trembling aspen
Buffalo berry
Common horsetail
Balsam poplar
Buffalo berry
Horsetail, grass
Buffaloberry
Fickle Lake Mixed
Fickle Lake Conifer
Cadomin Mixed
Cadomin Conifer
Prospect Creek
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Fig. 3 Selection of seasonal images acquired from the Cadomin conifer site
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Fig. 4 Standardized
curves showing growing
season trends in mean
daily temperature and the
global (image-wide)
2G-RBi index for the
Bryan Spur mixed site,
and noon sun elevation at
Robb, Alberta
and may be more sensitive to local variation
in canopy leaf area and chlorophyll concentrations
(Waring et al. 2006).
Once 2G-RBi values were calculated for each
region of interest within the images for the du-
Fig. 5 Graphic
representation of the
formulation of the mean
2G-RBi index through
the growing season, and
the field-based
phenocode values
ration of the observation period, curves were fitted to the data to estimate green-up and senescence. Using Landsat-derived indices, Fisher
et al. (2006) demonstrated that a logistic-growth
simulating sigmoid curve could be employed to
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Fig. 6 Example of
temporal sequence of
2G-RBI and phenocode
values for four
species-specific regions of
interest at three
vegetation sites in the
study area
estimate leaf onset and offset. The method was
improved upon by Soudani et al. (2008), who employed MODIS data to derive vegetation phenology dates. Similarly, using tower-based digital
images, Richardson et al. (2009) used two sigmoid functions multiplied together to fit curves
to relative channel brightness values observed by
the camera system, and then used the inflection
points to mark the beginning and end of the season in broadleaf and conifer forest canopies. In
this study, we adapted the method and used a
fourth-order polynomial function, rather than a
sigmoid, to fit the 2G-RBi observations throughout the observation period. Null and inflection
points were determined using the first, second and
third derivatives of the polynomial, and were used
to define the day of year of the initial green-up,
maximum greenness and end of the growing season. Using linear regression, statistical relationships were then developed between the human
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observed assessments of phenological phases and
the 2G-RBi data obtained from the speciesspecific regions of interest within the images.
Results
Over the installation period from 13 April 2009
to 27 October 2009, more than 6,700 images were
acquired across the seven sites. A 10% failure
rate was due largely to battery failure where light
levels below the canopy were not sufficient for
the camera units’ solar panels to maintain charge.
Figure 2 is a grayscale image example of the Bryan
Spur mixed site with regions of interest over three
understorey and one overstorey species. It is from
regions of interest such as these that the imagebased indices were calculated. Figure 3 shows
an example of images collected at the Cadomin
Conifer site, and indicates the variability of the
scenes with respect to the overstorey and understorey composition, as well as snow cover at the
commencement and end of the growing season.
Figure 4 shows fourth-order polynomials fit
to daily noon sun elevation angles at Robb, Alberta, and mean daily temperature and mean daily
scene-wide 2G-RBi at the adjacent Bryan Spur
mixed site. The trends indicate that the 2G-RBi
signal is related to temperature-induced changes
in plant phenology, and not simply a seasonal
fluctuation in scene brightness related to sun elevation angle.
Fig. 7 Results of the
linear regression analyses
using the camera-derived
2G-RBi as a predictor
variable. Predicted vs.
observed (left) start of
growing season (r2 =
0.61, df = 1, F = 14.3,
p = 0.0043) and (right)
length of growing season
(r2 = 0.72, df = 1, F =
23.09, p = 0.0009)
An example of a temporal sequence of mean
daily 2G-RBi values for a single region of interest,
and the species-specific phenological trajectory as
measured during field visits, is shown in Fig. 5. The
implementation of the half-maximum parameter
approach produced a range of start and end of
growing season dates across the 11 species-specific
regions of interest, and range from day 133 as
observed by the camera, through to day 190 as
observed from the field-based observations. Similarly, the growing season length as estimated using
the half maximum method ranged from 65 days
for the field observations, to 148 days using the
camera data. As would be anticipated, the start
of the growing season was generally later, and
length of growing season shorter, for high elevation sites (start of growing season mean = day 175,
length of growing season = 80 days) compared to
those at lower elevations (start of growing season
mean = day 170, length of growing season =
110 days).
Figure 6 shows additional examples comparing
the 2G-RBi calculated for species-specific regions
of interest to the field-based phenophase measurements for four species at three sites. On average, the first 2G-RBi half maximum inflection
points occurred 21 days before the beginning of
the growing season as observed in the field, while
the length of time between the first and last
half-maximums were 21 days greater than those
measured in the field. Based on linear regression
models, the relationship between the field and
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camera data indicates that 61% (r2 = 0.61, df =
1, F = 14.3, p = 0.0043) of the variance observed
in the field measures of phenological phases were
captured by the camera for the start of the growing season, and 72% (r2 = 0.72, df = 1, F = 23.09,
p = 0.0009) of the variance in length of growing
season (Fig. 7). The mean absolute differences in
residuals between predicted and observed start of
growing season and length of growing season were
4 and 6 days, respectively (Fig. 7).
Discussion and conclusion
The development of ground-based remote sensing networks, such as the one described in this
paper, provide the tools necessary for improving our understanding of the seasonal variations in vegetation phenology, and will ultimately
lead to improved detection of changing vegetation characteristics for wildlife management. In
addition, ground-based camera systems can provide high temporal resolution for calibration of
satellite-based monitoring initiatives. This study
expands on the previous work of others, such as
Richardson et al. (2007), Ahrends et al. (2008) and
Richardson et al. (2009), by demonstrating that
ground-based cameras can be employed to simultaneously monitor species-specific overstorey and
understorey phenology. In particular, the establishment of the network in a forest environment,
without the need for infrastructure such as a flux
tower, greatly improves flexibility.
Although growing season start and end dates
were successfully estimated using the halfmaximum approach, a limitation of working at
the plot scale was the inability to detect subtle
phenological events critical for wildlife habitat
(food) modelling. For instance, the precise timing of initial leaf unfolding or the development
of fruiting bodies was difficult to capture when
vegetation was at a distance from the cameras.
Further research is required to determine how
best to capture these events, and whether they
can be related to other phenological measures
that are easily observed at a distance. A possible
solution may be a more focused targeting of individual plants, and the investigation of possible
relationships between image-derived indices such
as the 2G-RBi, and biological events such as fruit
ripening. Placing cameras in greater proximity to
individual plants may also offer the advantage of
reduced frequency of field visits for collection of
phenological phase data, which could conceivably
be interpreted directly from the images.
Our results indicate that some biases exist between the timing of the half maximum and the
field-based estimates of growing season, which
was partly the result of differences in the nature
of the two data sets. The camera data provides
a daily indication of greenness, but is heavily
influenced by hourly, daily and seasonal changes
in illumination. The field observations, which are
based on weekly interpretations by ground crews
and account for overall leaf and plant condition,
are not quantitative measurements of changes in
plant biochemical composition. Nonetheless, the
cameras effectively captured a range of phenological conditions for multiple species found at the
sites along the transect, and the data they collect
represent both a spectral and visual record for
later use.
Grizzly bears use a variety of food resources
which are both seasonally and spatially dynamic.
Current wildlife models, however, lack the spatial
and temporal resolution to predict habitat use
at the scales in which animals respond to their
environment (Nielsen et al. 2010). A possible
solution may be the development of landscape
models with greater temporal and spatial resolutions using data fusion algorithms such as those
developed by Gao et al. (2006). Landsat, MODIS
or other remotely sensed information could then
be used to generate dense time-series representing
important phenological developments or stages
of critical food resources. Ground-based cameras
would thereby provide an important source of
information for model calibration or validation.
This is particularly important for habitats associated with rare species, such as grizzly bears, given
the difficulty of repeatedly visiting remote sites at
the frequency and quality necessary for detecting
changes in critical food resources. We suggest that
better spatially explicit predictions of the timing
of these events will lead to a better understanding
of relationships between climate, local and landscape patterns of food availability and quality, and
the responses of these changes and patterns by
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individual animals (e.g. body size and growth)
or populations. Critical to accomplishing this for
grizzly bears will be the integration of technologies, including satellite and ground-based remote
sensing platforms, to measure vegetation phenology; field and laboratory-based measures of nutrient quality in target plant foods; knowledge of the
distribution and abundance of food resources; the
behavioral responses of animals to environmental
changes; and measures of animal health or population dynamics. Linking these research elements
will ultimately lead to a broader understanding of
grizzly bear ecology and thus better management
and conservation of the species.
Acknowledgements Sam Coggins (University of British
Columbia) and David Laskin (University of Calgary)
were members of the deployment team. Karen Graham (Foothills Research Institute) and Tracy McKay
(Foothills Research Institute) were members of the
phenophase field monitoring team. Raphaël Roy-Jauvin
provided assistance with figures. Andrew Richardson
(Harvard University) and Scott Ollinger (University of
New Hampshire) provided initial advice and enthusiasm for the network plans. Funding for this research
was partially provided by the Grizzly Bear Program of
the Foothills Research Institute located in Hinton, Alberta, Canada, with additional information available at
http://www.foothillsresearchinstitute.ca/. Funding was also
provided by the Canadian Forest Service, the University
of British Columbia and an NSERC Discovery grant to
Coops.
Open Access This article is distributed under the terms
of the Creative Commons Attribution Noncommercial License which permits any noncommercial use, distribution,
and reproduction in any medium, provided the original
author(s) and source are credited.
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