Causes and Consequences of Ekwǫ̀ calving ground switching and shifts

Draft Report for WRRB

Author

Elie Gurarie, Benjamin Larue, Ophélie Couriot, Anne Gunn, Allicia Kelly

Published

September 9, 2026

1 Background

Barren-ground caribou across northern Canada are organized and managed as herds that are defined by the calving grounds they use each year Nagy et al. (2011). Female fidelity to these calving areas has long been treated as the basis for identifying population units and for guiding monitoring and harvest management (Gunn and Miller 1986, Gunn et al. 2017). This framework assumes that individuals consistently return to the same calving grounds year after year, which in turn maintains consistent separation among herds. This is generally an accurate characterization – as evidenced by copious empirical data and theoretical frameworks that emphasize the importance of sociality and gregariousness for caribou (Gunn et al. 2012). However, ever since individual cows could be identified and tracked for multiple years, we have known that herds are not closed populations and a low level switching calving grounds is typical fidelity by the majority of cows.

Telemetry data collected over the last two decades show that winter ranges used by neighboring herds often overlap. For example, the Western Arctic, Teshukpuk, Central Arctic and Porcupine Caribou herds in Alaska display both seasonal range overlap and herd interchange (Prichard et al. 2020). Among the Rivière Georges and Rivière-aux-Feuilles herds in northern Québec and Labrador, there is similarly considerable spatial overlap among these herds, including during the rut Boulet et al. (2007). In the central Canadian Arctic, Gurarie et al. (2023) documented highly variable winter overlap: at times very high (over 70%), at times near zero among all three major caribou herds, (Bluenose East, Bathurst and Beverly). These changes in spatial overlap can complicate herd-specific monitoring efforts because animals from different herds use the same landscapes during key periods of the annual cycle (Gurarie et al. 2023).

Collar data also show that calving-ground fidelity, while generally very high, can vary among individuals. In Alaska, up to 13% for the smaller herds (Teshekpuk and Central Arctic) calved with neighboring herds – what the authors refer to as “interchange”. This interchange, importantly, was strongly asymmetric: the large majority of switching events went from the two smaller herds to the two larger herds, with little flow in the reverse direction (Prichard et al. 2020). In northern Québec and Labrador, cross-herd interchange is at least high enough to cause there to be no genetic differentiation between the Rivière Georges and Rivière-aux-Feuilles herds (Boulet et al. 2007). Biologists monitoring caribou in the central Arctic document many cases of collared animals switching calving grounds - usually several a year. For example, between 1970 and 1979, based on 1300 marked caribou the switching rate between the Beverly and Qamanirjuaq calving grounds was 1.8% and 3.4%, respectively (Heard 1984). Campbell et al. (2019) reported 3 of 93 (3.1%) collared Bathurst animals switching to the Beverly range between 2010 and 2018, with none going the other way, though all of those occurred in the last year of monitoring (3 of 11 in 2018), with considerably more switching between Beverly and mainland Nunavut and Ahiak herds (10 of 116 out of Beverly, 7 of 26 into Beverly). Relatedly, considerable debate surrounds the identity of Ahiak and Beverly herds. For example an argument made that the entire distinct Beverly herd – which traditionally calved in the interior of northern Nunavut near Beverly Lake – had been absorbed into the Ahiak herd (with a more coastal calving range) as the consequence of a herd-level population decline, possibly accelerated by large-scale herd switching between mid-1990’s and 2011 (Adamczewski et al. 2015). Collectively, these animals are generally refered to as Beverly, while Ahiak animals are now considered to animals calving on the coast further east along the Arctic coastline. These observations across the North American migratory caribou range point to the dynamic nature of herd association and identity, and to the role that both shifting between calving ranges, and the shifting of calving ranges themselves, play in herd structures.

Since 2017, a significant number of collared females from the greatly diminished Bathurst herd have migrated to the east coast of Bathurst Inlet during the pre-calving period, an area situated outside the presently recognized Bathurst calving ground but documented as a calving region for Bathurst animals until the mid-1990s Gunn et al. (2012). Herd switching rates, in and out of the Bathurst, Bluenose East and Beverly herds, have apparently also been on the rise. Our immediate goals in this report is to: (1) Quantify the switching rates among these herds; (2) assess whether winter associations between herds lead to a higher rate of calving ground switching; and (3) assess whether animals travel together share common destinations. The collected information to determine whether social interactions may be increasing the likelihood of herd switching and thus slowing the recovery of the Bathurst population, and provide evidence for or against a “socially mediated Allee affect”, i.e. the notion that social interactions among herds during non-calving seasons can accelerate the numeric decline of a highly depleted herd. Improved understanding of the causes and consequences of calving-ground switching is essential for interpreting population trends, coordinating management across regions, and supporting conservation planning for migratory caribou.

2 Defining and Estimating Calving Ground Switches

2.1 Methods

2.1.1 Coastal Areas

We took a purely spatial approach to classifying the calving ground association of each animal in each year, more or less following the techniques introduced by (Nagy?). We delineated 7 greater calving ground areas (Figure 1). For most coastal areas, the herd association is very clear. These include the Tuktuyaktuk Peninsula (TUK) and Cape Bathurst (CBT). Bluenose West and Bluenose East herds are also fairly well clustered in the respective coastal areas (BLW and BLE). The Bathurst herd is mainly associated with animals that calved in the Bathurst Inlet West (BIW) coastal area, but also some animals that calved east of Bathurst Inlet (BIE). Beverly herd animals are mainly captured by the Queen Maud Gulf (QMG); a very large area which shifts considerable across years.

A few animals are in the Northeast Mainland coastal area (NEM) - belonging to the Wager Bay and Lorillard herds which are largely outside the scope of our analysis. Animals found outside of any of the coastal areas are either individuals that likely didn’t make it to the calving ground, or may belong to the Qamanirjuaq herd that calves near Baker Lake in Eastern Nunavut.

Figure 1: Coastal Areas, defined as per the table in the text. Points indicate the location of female caribou on June 3 from all years of sampling (1996-2025) - bluer colors are older, redder colors are more recent.

2.1.2 Classifying individual caribou by peak calving date

We used data from female caribou instrumented with GPS collars by the Government of Northwest Territories (n = 1354, animal years = 3316). While our focus of these analyses is on the three major eastern herds (Bluenose East, Bathurst and Beverly), accounting for all the herds allows us to also consider movements into and out of this core group.

Collaring efforts in NWT date back to 1996, but the sample sizes increased significantly after 2006 (Figure 2). Migration timing (Gurarie et al. 2019) and calving timing (Couriot et al. 2023) can vary considerably across years and among individuals among these herds. We estimated the calving time using the method of Couriot et al. (2023) for all the animals since 2006 (detailed results in Appendix B, Table 8 and Figure 20.). While there is a distinct west to east gradient in mean calving days (e.g. May 28 for Tuktuyaktok Peninsula, to June 6 for Beverly), the overall peak calving date across animals was June 3 (SD 7.5 days). We therefore assigned each individual to the coastal area of each individual on June 3. Since animals first arrive before calving if possible, and typically spend around a week with their calves before moving, this date should largely capture those animals still on the calving grounds after giving birth, and those on or near the calving ground before giving birth. The large size of the coastal areas also help absorb much of the variation in movement activity across animals. Note also, that whereas we use the calving locations of likely parturient females, our goal is to have a flexible method to classify all the females, not all of which reproduce, but many of which also migrate to calving grounds due to the strong social behaviors of these herding animals.

On balance, we feel that combining coastal areas with peak calving is a parsimonious and generally reliable method to classify all female caribou that is consistent with other common classifications, for example Nagy et al. (2011), and as currently conducted by the GNWT. One immediate issue that arises is the ambiguity of the “Bathust Inlet East” coastal area, as it straddles the very elongated and relatively more dynamic Beverly (formerly, Ahiak) calving grounds while being not too far from the current Bathurst Herd calving grounds, yet squarely overlapping with the areas that were formerly the core calving ground of the Bathurst herd. This is an area of ecological importance that appears to be increasingly used, even as the Bathurst and Beverly animals are appearing to mix. We embrace the ambiguity of this area by giving it its own designation. We also provide a detailed analysis of animals that appear to have calved in this area below (Section 2.2.3).

Table 1

Code

Coastal Area

Herd(s)

n

%

TUK

Tuktoyaktuk Peninsula

Tuktoyaktuk Peninsula

249

7.5

CBT

Cape Bathurst

Cape Bathurst

514

15.5

BLW

Bluenose Lake West

Bluenose West

669

20.2

BLE

Bluenose Lake East

Bluenose East

782

23.6

CG

Coronation Gulf

Bluenose East or Bathurst

16

0.5

BIW

Bathurst Inlet West

Bathurst

471

14.2

BIE

Bathurst Inlet East

Bathurst or Beverly

36

1.1

QMG

Queen Maud Gulf

Beverly or Ahiak

493

14.9

NEM

Northeast Mainland

Lorrilard or Wager Bay

14

0.4

OUT

Outside

Any of above - or Qamanirjuaq

72

2.2

Figure 2: Number of collared individuals in coastal area on June 3 by year.
Figure 3: Collared animal calving area locations on June 3 across years (since 2006). Note that starting in 2021, nearly all of the collars were collared from west of Bluenose Lake eastward.

2.1.3 Comparing to overall population size

When considering these numbers, it is important to recall that the absolute sizes of these populations are very different, and that they have changed considerably across years. The NWT conducts aerial surveys and reports estimates of these populations with some regularity. We use those reported estimates to obtain interpolated and smoothed estimates of population size across years for each herd, using Generalized Additive Models (GAMs). The results are shown in Figure 4, and the methods are described in detail in Appendix C. In calculations of herd transitions, we will use these estimates as the baseline source populations to obtain coarse estimates of absolute numbers of individuals switching herds. These herds will correspond to their principal coastal areas, i.e. (skipping the self-evident Tuktoyaktuk Peninsula, Cape Bathurst, Bluenose Lake West and Bluenose Lake East), the Bathurst Herd will be associated with source populations from Bathurst Inlet West, and Beverly Herd animals will be associated with source populations from the Queen Maud Gulf coastal area.

Figure 4: Predictions of population size for each herd across years, with 95% confidenct intervals (curves and shaded ribbons). Dark grey points and error bars indicate observed estimates and 95% CIs from aerial surveys. Note different scales for western herds (top row) and eastern herds (bottom row).

2.2 Results

2.2.1 Overall summaries

A complete accounting of all collared females with their coastal area associations and transitions is provided in Table 2, together with a highly approximate accounting of the actual total number of animals that may have switched.

Across all herds and years, the large majority of collared females returned to the same calving area as the previous year. Of 1492 total year-to-year transitions recorded, 1412 (94.6%) were to the same area, while 80 (5.4%) involved a switch to a different calving ground. Most switching occurred between neighboring areas — most commonly between BLE and BLW, and between CBT and TUK. More notable are movements into atypical areas distant from the main herd ranges. Bathurst Inlet East (BIE) and Coronation Gulf (CG) together account for 20 switching events: 13 to BIE (almost exclusively among Bathurst and Beverly animals) and 7 to CG (primarily Bluenose-East animals).

Of note are switching into areas that do not correspond to known or traditional calving grounds, in particular Coronation Gulf (CG) and East of Bathurst Inlet (BIE). These transitions have also been most pronounced for the Bathurst herd, and in recent years. In 2017, 50% of tracked Bathurst females did not return to BIW — the highest single-year rate in the dataset — with animals moving to both QMG and BIE. Departures from BIW recurred in most subsequent years through 2023. For Beverly, BIE destinations appeared sporadically through 2009 and again from 2018 onward.

2.2.2 Absolute numbers

These figures can be expressed in approximate absolute numbers by weighting each observed transition by the contemporaneous herd population estimate, though these estimates carry substantial uncertainty — population surveys are infrequent, collar sample sizes are small, and the expansion from collared individuals to herd-wide totals compounds these errors considerably. The numbers below should therefore be treated as rough indicators of order of magnitude rather than precise counts.

With those caveats, movements to BIE across the full study period represent an estimated 78,085 animal-years (95% CI: 69,384–86,786), the large majority attributable to Beverly animals (74,950; CI: 67,940–81,960). Movements to CG represent an estimated 10,687 animal-years (CI: 9,449–11,925). For the Bathurst herd in 2017 — the year of peak switching — the estimated 4,845 animals departing BIW (CI: 2,454–7,236) should be viewed in the context of the herd’s already greatly reduced total of approximately 9,690 animals at that time.

Table 2: Table of calving area transitions among coastal areas for the Bluenose East, Bathurst, and Beverly herds from 2006 to 2025. For each year and source herd, the number of observed transitions (n), percentage of total transitions (%), and estimated number of animals (Est.) are provided for each destination coastal area.

BLW

BLE

CG

BIW

BIE

QMG

Year

n

%

Est. (×1000)

n

%

Est. (×1000)

n

%

Est. (×1000)

n

%

Est. (×1000)

n

%

Est. (×1000)

n

%

Est. (×1000)

Bluenose-East

2,006

1

12.5

15.1

7

87.5

105.8

2,007

8

100

120.1

2,008

16

100

121.4

2,009

25

96.2

118.1

1

3.8

4.7

2,010

1

6.2

7.4

15

93.8

111.4

2,011

5

100

105.9

2,012

22

100

87.6

2,013

1

6.7

4.6

14

93.3

64.1

2,014

11

100

51.6

2,015

16

100

38.9

2,016

26

100

30

2,017

1

5.9

1.5

16

94.1

23.3

2,018

19

95

21.1

1

5

1.1

2,019

11

91.7

19.8

1

8.3

1.8

2,020

24

100

22.7

2,021

3

6.5

1.7

43

93.5

23.9

2,022

30

90.9

27.3

2

6.1

1.8

1

3

0.9

2,023

1

2.6

0.9

35

92.1

32.5

1

2.6

0.9

1

2.6

0.9

2,024

2

5.6

2.2

32

88.9

34.8

1

2.8

1.1

1

2.8

1.1

2,025

39

100

40.8

Bathurst

2,006

2

100

126.1

2,007

5

100

80.9

2,009

6

85.7

36.2

1

14.3

6

2,010

1

14.3

5

6

85.7

29.9

2,011

7

100

30.9

2,012

10

100

27.5

2,013

3

100

23.9

2,014

12

100

19.8

2,015

20

100

15.9

2,016

20

100

12.4

2,017

6

54.5

5.3

2

18.2

1.8

3

27.3

2.6

2,018

11

84.6

6.4

2

15.4

1.2

2,019

7

100

6.4

2,020

27

81.8

4.7

5

15.2

0.9

1

3

0.2

2,021

20

95.2

5.2

1

4.8

0.3

2,022

14

77.8

4.2

4

22.2

1.2

2,023

1

6.2

0.3

1

6.2

0.3

11

68.8

3.6

3

18.8

1

2,024

8

88.9

4.4

1

11.1

0.6

2,025

12

100

4.3

Beverly

2,006

8

100

137.6

2,007

2

22.2

30.5

7

77.8

106.8

2,008

1

12.5

17.1

7

87.5

119.8

2,009

1

7.1

9.7

1

7.1

9.7

12

85.7

116.8

2,010

8

100

135.3

2,011

3

100

133.3

2,012

6

100

130.2

2,013

4

100

126

2,014

22

100

121.5

2,015

20

100

117.2

2,016

12

100

114.3

2,017

15

100

112.3

2,018

1

7.1

8

1

7.1

8

12

85.7

96.5

2,019

9

100

116.3

2,020

1

10

12.3

9

90

110.7

2,021

1

11.1

14.5

8

88.9

116.3

2,022

11

100

137.5

2,023

1

3.3

4.8

29

96.7

138.8

2,024

1

5

7.5

1

5

7.5

18

90

134.8

2,025

10

100

153.7

2.2.3 Focus on East of Bathurst Inlet

The sequence of images below focus on a important subset of animals (\(n=8\)) that calved east of Bathurst Inlat, in an area what was largely considered not to be the current calving ground of either Bahurst or Beverly herd animals. Of note: all but one of those animals were clearly Bathurst animals in the preceding year, and none of those animals ever returned to calve in that calving area.

Figure 6: In 2021, all but one animal clearly calved west of Bathurst Inlet, in traditional Bathurst calving grounds, the last was a Beverly animal (red dot -caribou BGCA19354) that wintered near the other animals.
Figure 7: In 2021, the animals passed took various routes - a few through the Bathurst calving grounds, but moved on to BIE to (presumably) calve.
Figure 8: Post-calving movements scattered widely, including the original Beverly animal moving up to the estern extreme of the Queen Maud Gulf.
Figure 9: Wintering grounds in 2021
Figure 10: Following year (2022) migration to widely scattered areas, none of which were traditional Bathurst calving grounds (BIW).
Figure 11: color legend of IDs

3 Predictors of Herd Switching

3.1 Spring sociality and nearest neighbors

To evaluate whether social associations during the pre-calving period influence a female’s decision to switch calving areas from one year to the next, we computed two complementary metrics of spring sociality from the daily GPS locations of collared females during the March 1–April 15 pre-calving window. This timing window corresponds to the period just before most animals are actively moving toward calving grounds and are still on wintering grounds. We tested whether this period could correspond to a critical time when social bonds and movement decisions are likely to interact and influence each individual’s current year coastal calving location choice.

For each focal female, we identified its nearest neighbor: the individual with the smallest mean daily separation distance across the whole pre-calving window. The rationale for this metric is that a single, consistent close associate is could provide strong directional social information, potentially leading or reinforcing movement toward a particular calving area. We recorded both the identity and the coastal calving area of this nearest neighbor, allowing us to ask whether the neighbor’s calving affiliation predicted whether the focal animal switched its own calving area the following year.

3.1.1 Nearest neighbor over time

We identified the nearest neighbor for each female caribou every day from April 1 to June 3, and identified whether the nearest neighbor was from the same herd or not, and whether each individual changed herds. The general temporal pattern of nearest neighbor association against switching is illustrated in Figure 12. The probability that a nearest neighbor was from a different herd was as high as 40% for non-switchers (the vast majority of animals), and tended to decrease during the animal migration as expected. For animals that did switch, however, the probability that the nearest neighbor was from a different herd tended to be higher throughout April.

Figure 12: Proportion of caribou days in which the nearest neighbor originated from a different coastal area, plotted against day of year from April 1 to June 3. Points represent daily proportions pooled across all animals within a year, sized by the number of contributing neighbor-days and colored by year. Curves are binomial GAM fits with 95% confidence ribbons, fit separately to animals that switched calving grounds (blue) and those that returned to the same coastal area as the previous year (black). Note that the late-season divergence reflects the fact that switching has already occurred.

3.1.2 April Nearest neighbor

We focused on April as a predictor of switching, identifying the consistent nearest neighbor (within 10km) for each individual throughout the month. Overall, over 25% (419/1640) of all animals originating in BNE, BIW and QMD had nearest April neighbors from different coastal area, and animals whose nearest neighbor came from a different coastal area were roughly twice as likely to switch calving grounds the following year (39/419 = 9.3%) compared to those whose nearest neighbor was from the same coastal area (60/1221 = 4.9%), a highly significant difference. This association was partially confounded by origin: Bathurst animals (originating in BIW) were both disproportionately likely to have a nearest neighbor from a different herd (35.4%, vs. 22.1% for BLE and 21.9% for QMG) and disproportionately likely to switch overall.

Table 3: Proportion of animals that switched herds, contrasting those whose nearest neighbor were from the same herd or from a different herd.

Herd

Nearest Neighbor

N

Switched

% Switched

Bluenose West

Same herd

282

4

1.4%

Different herd

12

0

0.0%

Bluenose East

Same herd

293

13

4.4%

Different herd

68

5

7.4%

Bathurst

Same herd

119

13

10.9%

Different herd

62

11

17.7%

Beverly

Same herd

36

1

2.8%

Different herd

28

2

7.1%

3.1.3 April Nearest Neighbor as predictor of switching

We modeled the probability of calving ground switching as a function of the coastal-area identity of an individual’s nearest neighbor in April (same vs. different coastal area) and origin coastal area, using generalized linear mixed models with a binomial response. Analysis was restricted to individuals originating in the Bluenose-East (BLE), Bathurst (BIW), and Beverly (QMG) coastal areas. Year was included as a random intercept in a subset of models to account for unstructured annual variation in switching probability. A candidate set comprising origin herd, origin herd and nearest-neighbor status (same or different), their interaction, and the same models with year as a random effect was compared using AIC (Table 4).

Table 4: AIC comparison of candidate models for calving ground switching.

Model

k

AIC

BIC

Herd + Re(Year)

5

518.8

544.8

Herd + NN + Re(Year)

6

519.5

550.7

Herd + NN

5

523.3

549.3

Herd x NN

8

526.0

567.6

Herd

4

526.1

546.9

On balance (perhaps surprisingly), the April nearest neighbor effect was negligible in predicting the probability of switching. E.g., for the best model that included the nearest neighbor effect the estimated coefficient was 0.37 (se. 0.31, p-value 0.24), which corresponds to an increased probability of switching of only 1.9% (C.I.: -0.95% - 5.9%).

Figure 13: Estimated change in calving ground switching probability when the April nearest neighbour was from a different coastal area for each herd (mean ± 95% CI; dashed line = no effect).

Take-away: April nearest neighbor associations are WEAK predictors of herd switching.

3.2 Winter social mixing

We also modeled the role of overall winter mixing across herds in predicting whether an individual switches herds. To do this, we computed a cross-herd mixing index for winter (December through March). For each individual for each day across the period, we drew a 10km radius and simply counted the proportion of animal-days from different herds (i.e. that calved in other coastal areas) divided by the total number of animal-days within the radius. The index ranges from 0 for animals that are entirely surrounded by animals from the same herd, to 1 for animals surrounded entirely by animals from other herds. We then used this mixing index as a predictor of herd-switching in a set of models, similar to the approach used for the nearest neighbor analysis above.

3.2.1 Results

We obtained social mixing indices from 1092 animal winters between 2005 and 2025. We focussed on Bluenose West, Bluenose East, Bathurst and Beverly herds(and included those animals that apparently calved in the intermediate coastal areas of Coronation Gulf and East of Bathurst Inlet. Nearly half the animals (48%, 525/1092) were in at least somewhat mixed groups, and 17% of all animals (208/1092) were in highly mixed groups, where over 70% of the individual-days within a given radius were from other herds.

As shown in Figure 14 and Table 5, winter social mixing varied strongly across herds. The Bluenose West herd (BLW) mixed less than any other (69% no mixing, 24% low mixing), while Bathurst animals mixed most (69% at least some mixing, and 32% high mixing).

Figure 14: Winter social mixing among collared female caribou by calving ground of origin for six coastal areas arranged west to east. Grey rectangles represent the proportion of animals that showed 0 mixing during the winter (i.e. no animals within 10 km originated from different herds). Light blue, blue and purple rectangles represent increasingly higher levels of mixing (e.g. animals that calved in Coronation Gulf and Bathurst Inlet East - not traditional calving grounds - were primarily surrounded by animals from other calving grounds the following winter, as expected). The total areas of the rectangles are proportional to the sample sizes.
Table 5: Social mixing index in the winter after calving for animals from 6 coastal areas, and sample sizes.

Winter social mixing

Coastal area

n

None
(m = 0)

Low
(< 0.3)

Medium
(0.3–0.7)

High
(> 0.7)

BLW

310

69%

24%

2%

5%

BLE

391

52%

18%

13%

16%

CG

9

0%

0%

0%

100%

BIW

206

31%

11%

27%

32%

BIE

11

0%

0%

0%

100%

QMG

165

51%

7%

17%

25%

The extent of social mixing appears to have increased over time, as evidenced in the contrast between overall social mixing in the years prior to and since 2016 (Figure 15). In both cases, Bathurst animals (BIW) are the most socially mixed, but the increase across years was marked, and cut across all herds. Most dramatically among Beverly animals (QMG), where the number of animals in mixed groups increased from 9% of animals (5/54), to 68% of animals (76/111).

Figure 15: Marked shift in social mixing contrasting years before 2016 and since 2016.

We assessed trends in social mixing over time by fitting beta-binomial models on the number of animal days from different coastal areas against animal-days from within the same coastal area against combinatinos of coastal area and Year - to assess any trends. We also included the total number of individual-years within the 10 km radius in the model, as larger samples were more likely to have some mixing.

Model

AIC

df

ΔAIC

AIC weight

Area x Year + log(N)

4,554.7

10

0.0

0.99

Area + Year + log(N)

4,564.4

7

9.7

0.01

Area + log(N)

4,588.6

6

33.9

0.00

null

4,715.0

2

160.3

0.00

log(N)

4,715.0

3

160.3

0.00

Coastal area

n

Mean m

Year trend (± SE)

φ

Bluenose West

310

0.09

0.056 ± 0.022

*

0.72

Bluenose East

391

0.25

0.031 ± 0.018

0.41

Bathurst

206

0.43

0.097 ± 0.029

***

0.66

Beverly

165

0.33

0.155 ± 0.036

***

0.77

* p < 0.05, ** p < 0.01, *** p < 0.001

Take-away: Social mixing is high and generally increasing (even accounting for sampling).

3.2.2 As predictor of switching

Figure 17: Predicted probability (dark lines) and 95% confidence intervals (shaded area) of calving ground switching as a function of mixing index for four herds of caribou.

Coastal area

n

% switched

m effect (SE)

p value

BLW

290

3.4%

3.93 (1.07)

< 0.001

***

BLE

354

4.3%

4.35 (0.94)

< 0.001

***

BIW

182

11.5%

1.87 (0.83)

0.024

*

QMG

150

6.8%

2.02 (0.83)

0.015

*

* p < 0.05, ** p < 0.01, *** p < 0.001

Figure 18: Predicted change in calving ground switching probability when winter social mixing ranges from minimum (m = 0) to maximum (m = 1) for each herd (mean ± 95% CI; dashed line = no effect).

Take-away: Across ALL herds, winter social mixing is a very strong predictor of herd switching. But, surprisingly, weakest for the Bathurst herd.

3.3 Repeat Switching

To answer the question of whether an animal that previously switched is more likely to switch, we cross-tabulated animal history against whether the animal switched in the current yea. We did this separately for all herds (i.e. excluding CG and BIE due to insufficient sample size). For each coastal area × prior-switching-history combination, we estimated the probability of switching with a Wilson score 95% confidence interval (prop.test, R v4.x) to account for some small sample sizes. Switching probabilities were compared descriptively between previously-switched and never-switched animals within each coastal area. As per the Figure 19 and (tab-priorswitch?), prior switchers on average were much more likely to switch than animals that had never switched. We can therefore consider that the tendency to switch herds is in some ways an intrinsic of individual caribou.

Figure 19: Probability of switching calving ground in a given year, by prior switching history and coastal area (point size = sample size; error bars = 95% CI).
Table 6: Switching frequency by coastal area for animals that have never switched versus those that have previously switched, with 95% confidence intervals.

Never Switched

Previously Switched

Coastal Area

N

N Switched

% Switched (95% CI)

N

N Switched

% Switched (95% CI)

TUK

133

5

3.8 (1.4-9.0)

15

7

46.7 (22.3-72.6)

CBT

306

5

1.6 (0.6-4.0)

10

8

80.0 (44.2-96.5)

BLW

365

4

1.1 (0.4-3.0)

20

9

45.0 (23.8-68.0)

BLE

410

8

2.0 (0.9-4.0)

24

12

50.0 (31.4-68.6)

BIW

215

13

6.0 (3.4-10.4)

18

13

72.2 (46.4-89.3)

QMG

229

6

2.6 (1.1-5.9)

13

6

46.2 (20.4-73.9)

4 Discussion

4.1 To-Do’s

  • Sensitivity to selected time ranges:
    • mixing: Dec / Jan / Feb / March / April(?)
    • [stability of winter mixed groups] seems like separate question … likely little bearing on high-level result of importance as predictor
  • Years since collaring as predictor: Definitively Non-Significant (very high p-values)

Other things to look at (maybe):

  • Distance from core of calving ground [centroid of locations, density of use (perhaps multiplied by population size - normalize to “true” density)]

    • PREDICTION: caribou that calve closer to the core, are LESS likely to SWITCH
  • Use a Herd-Year specific peak calving date - collective lowest movement rate day between June 1 and June 15.

  • Distance to new / old calving ground

  • Distance from where wintered the previous year

5 References

Adamczewski, J., A. Gunn, J. Nishi, K. Poole, and J. Boulanger. 2015. What happened to the Beverly caribou herd after 1994? Arctic 68:407–421.
Boulet, M., S. Couturier, S. D. Côté, R. D. Otto, and L. Bernatchez. 2007. Integrative use of spatial, genetic, and demographic analyses for investigating genetic connectivity between migratory, montane, and sedentary caribou herds. Molecular Ecology 16:4223–4240.
Campbell, M., D. Lee, and J. Boulanger. 2019. Abundance trends of the beverly mainland migratory subpopulation of barren-ground caribou (Rangifer tarandus groenlandicus): June 2011 – june 2018. Technical {{Report Series}}, Government of Nunavut Department of Environment.
Couriot, O. H., M. D. Cameron, K. Joly, J. Adamczewski, M. W. Campbell, T. Davison, A. Gunn, A. P. Kelly, M. Leblond, J. Williams, W. F. Fagan, A. Brose, and E. Gurarie. 2023. Continental synchrony and local responses: Climatic effects on spatiotemporal patterns of calving in a social ungulate. Ecosphere 14.
Couturier, A. S., J. Brunelle, D. Vandal, and G. St-Martin. 1989. Changes in the population dynamics of the george river caribou herd, 1976-87. Arctic 43:9–20.
Gunn, A., and F. L. Miller. 1986. Traditional behaviour and fidelity to caribou calving grounds by barren-ground caribou. Rangifer, Special Issue: 6:151–158.
Gunn, A., K. G. Poole, and J. S. Nishi. 2012. A conceptual model for migratory tundra caribou to explain and predict why shifts in spatial fidelity of breeding cows to their calving grounds are infrequent. Rangifer:259–267.
Gunn, A., K. G. Poole, D. E. Russell, Canada, Environment and Climate Change Canada, and Committee on the Status of Endangered Wildlife in Canada. 2017. COSEWIC assessment and status report on the caribou, Rangifer tarandus, barren-ground population, in Canada. COSEWIC, Committee on the Status of Endangered Wildlife in Canada, Ottawa.
Gunn, A., K. G. Poole, and J. Wierzchowski. 2008. A geostatistical analysis for the patterns of caribou occupancy on the Bathurst calving grounds 1966–2007. Contract Report, Indian and Northern Affairs Canada, Yellowknife, NWT.
Gurarie, E., A. Gunn, O. Couriot, and A. Guile. 2023. Annual variation in the seasonal range overlap between the Bathurst, Bluenose East, and Beverly caribou herds. Contract Report, Wek’èezhìı Renewable Resources Board.
Gurarie, E., M. Hebblewhite, K. Joly, A. Kelly, J. Adamczewski, S. Davidson, T. Davison, A. Gunn, M. Suitor, W. Fagan, and N. Boelman. 2019. Tactical departures and strategic arrivals: Divergent effects of climate and weather on caribou spring migrations. Ecosphere (Washington, D.C) 10.
Heard, D. C. 1984. Hunting patterns and the distribution of the Beverly, Bathurst and Kaminuriak caribou herds based on the return of tags by hunters. Page 49. File {{Report}}, Northwest Territories Wildlife Service, Yellowknife, N.W.T.
Nagy, J. A., D. L. Johnson, N. C. Larter, M. W. Campbell, A. E. Derocher, A. Kelly, M. Dumond, D. Allaire, and B. Croft. 2011. Subpopulation structure of caribou (Rangifer tarandus L.) in arctic and subarctic Canada. Ecological Applications 21:2334–2348.
Prichard, A. K., L. S. Parrett, E. A. Lenart, J. R. Caikoski, K. Joly, and B. T. Person. 2020. Interchange and Overlap Among Four Adjacent Arctic Caribou Herds. The Journal of Wildlife Management 84:1500–1514.

Appendix

APPENDIX A: Total number of animals in each coastal area by Year

Table 7

Year

TUK

CBT

BLW

BLE

CG

BIW

BIE

QMG

NEM

Outside

1996

0

5

4

5

0

9

0

0

0

0

1997

0

4

5

5

0

6

0

0

0

1

1998

0

3

5

5

0

1

0

0

0

0

1999

0

7

12

4

0

7

0

0

0

0

2000

0

2

1

3

0

2

0

0

0

1

2001

0

0

0

0

1

0

0

0

0

1

2003

0

8

3

0

0

0

0

0

0

0

2004

0

2

2

0

0

1

0

0

0

0

2005

0

8

9

7

0

1

0

0

0

1

2006

8

11

16

12

0

3

0

11

0

7

2007

5

19

19

10

0

9

0

12

0

2

2008

10

22

24

25

0

7

3

18

1

18

2009

18

23

42

38

1

12

1

22

1

7

2010

12

12

25

39

2

20

2

18

0

9

2011

9

8

13

17

0

18

0

12

0

1

2012

16

21

39

45

0

19

1

21

0

3

2013

12

10

28

24

0

12

0

7

3

4

2014

7

14

18

21

0

16

0

29

0

1

2015

18

40

38

24

0

31

0

32

0

1

2016

6

27

33

35

0

27

0

21

2

0

2017

3

25

17

31

0

31

0

24

1

2

2018

10

33

42

30

0

15

5

29

1

2

2019

5

20

20

28

3

24

5

26

0

3

2020

5

16

11

34

1

38

0

12

0

4

2021

13

44

49

62

0

39

12

23

0

0

2022

9

29

38

54

2

37

2

19

0

0

2023

8

26

29

56

3

29

1

57

0

1

2024

34

43

53

56

2

18

0

34

1

1

2025

22

21

51

60

1

24

3

26

2

2

2026

19

11

23

52

0

15

1

40

2

0

APPENDIX B: Calving dates across herds

We applied the method developed in (Couriot et al. 2023) and applied it to all data through 2025 to obtain a mean and standard error of calving dates by each coastal area. Summary results below.

Table 8

Coastal Area

No.

%

No.

%

Peak date

Tuktoyaktuk Peninsula

52

60

35

40

27 May ± 7.1

Cape Bathurst

158

74

56

26

31 May ± 7.9

Bluenose Lake West

363

82

77

18

02 Jun ± 6.8

Bluenose Lake East

435

88

57

12

05 Jun ± 6.9

Coronation Gulf

11

92

1

8

08 Jun ± 8.3

Bathurst Inlet West

231

77

69

23

02 Jun ± 5.9

Bathurst Inlet East

19

76

6

24

08 Jun ± 7.9

Queen Maud Gulf

260

83

53

17

05 Jun ± 6

Northeast Mainland

8

100

0

0

05 Jun ± 4.7

Figure 20: Violinplot of estimating calving date based on movement analyses across the 9 coastal areas. The widths of the violins is proportional to the sample size, also reported across the top.

APPENDIX C: Population Interpolation

Raw numbers of caribou population estimates for the NWT herds were obtained from GNWT-ECC surveys. These surveys are typically conducted every 3-5 years using aerial photography methods, with associated uncertainty estimates (standard errors or confidence intervals). The data span from 2006 to 2025, with some herds having earlier or later initial surveys. Raw population data for the herds are plotted below:

Figure 21: Observed population estimates (points) with 95% confidence intervals (error bars) for six NWT herds from 2006 to 2025.

We interpolated and extrapolated these estimates over the complete period 2006-2025 using generalized additive models (GAMs) fitted independently for each herd. We modeled observed population counts \(N_t\) at time \(t\) as:

\[\log(\mathbb{E}[N_t]) = f(t)\]

where \(f(t)\) is a thin-plate regression spline with basis dimension \(k = \min(5, \lfloor 0.8n \rfloor)\), and \(n\) is the number of observations for that herd. The log link ensured positive predictions. Models were fitted using restricted maximum likelihood (REML) via the mgcv package in R (mgcv?).

For herds where survey data began after 2006 (e.g., Bluenose-East: 2010, Beverly: 2011), we imputed values for the missing early years using the earliest available observation. These imputed points—carrying the same estimate and uncertainty as the first survey—were included as input data for model fitting. This assumes approximate population stability prior to the first survey and anchors the spline during periods without observations.

To ensure prediction intervals reflect observation-level uncertainty, we used a parametric bootstrap. For each of 500 iterations:

  1. Observed population estimates (including imputed early values) were resampled from \(N(\hat{N}_t, \text{SE}_t^2)\), where \(\text{SE}_t\) is the reported standard error. For observations lacking reported uncertainty, SE was imputed using the median coefficient of variation (CV) across observations with known SE for that herd. Resampled values were floored at 100 to prevent negative or near-zero populations.

  2. A GAM was fitted to the resampled observations.

  3. Predictions were extracted for each year in 2006–2025.

Prediction intervals were computed as the 2.5th and 97.5th percentiles of the bootstrap distribution, with point estimates taken as the median. This approach ensured that (a) prediction uncertainty is at least as large as observation uncertainty, (b) the predicted trajectory respects the range of plausible values given the original confidence intervals, and (c) uncertainty in data-sparse periods was appropriately inflated.

This is a fairly conservative approach to intra/extrapolating population estimates. It assumes:

  1. That population trajectories are reasonably smooth functions of time with high autocorrelation. An inspection of the raw data seems to support this assumptions, though the smooth fails account for a high Tuktoyaktuk Peninsula estimate in 2021 and a low Bathurst one in 2009 for example.

  2. For lack of other information, we assume a constant population prior to the first observation (i.e. between 2006 and the next reported estimate), and after the last observation (until 2025). This is a placeholder reflecting absence of information rather than ecological expectation. This means the Beverly and Bluenose East predictions prior to their first reported estimates (2011 and 2010, respectively) may be underestimates, and the apparent uptick in Bluenose East and Beverly numbers is also slowed.

  3. Early surveys often lack reported uncertainty. The CV-based imputation assumes these observations have comparable relative precision to later surveys.

The resulting predictions are plotted in figure Figure 4 and tabulated in table Table 9 below. The code to replicate these predictions are in the TuktuData package (available upon request).

Table 9: Predicted caribou population estimates (x1000) with 95% CI.

Year

Tuktoyaktuk Peninsula

Cape Bathurst

Bluenose-West

Bluenose-East

Bathurst

Beverly

2,006

3.3 (2.5–3.9)

2.6 (1.8–3.3)

27 (22.6–31.3)

120.9 (110.4–131.6)

126.1 (73.2–185)

137.6 (126.8–147.6)

2,007

3.1 (2.5–3.6)

2.6 (1.9–3.1)

26.6 (22.8–30.6)

120.1 (113.3–127.3)

80.9 (54.4–119.8)

137.3 (130.4–144.1)

2,008

2.9 (2.5–3.3)

2.6 (2–3.1)

26.1 (22.4–30.1)

121.4 (114.1–128.7)

55.1 (37.1–81.8)

136.9 (131–144.5)

2,009

2.7 (2.4–3.1)

2.6 (2.1–3)

25.7 (22.3–30)

122.8 (115.9–129.3)

42.2 (27.3–58.2)

136.3 (130.9–144.2)

2,010

2.6 (2.2–2.9)

2.6 (2.2–3)

25.4 (21.8–30.3)

118.8 (109.5–127.7)

34.9 (26.1–43.9)

135.3 (128.6–143.3)

2,011

2.5 (2.1–2.8)

2.6 (2.3–3)

25 (21.2–31.3)

105.9 (94.5–119)

30.9 (22.6–39.2)

133.3 (124.8–142.6)

2,012

2.3 (2–2.7)

2.7 (2.3–3.1)

24.5 (20.7–32.4)

87.6 (77–102.1)

27.5 (16.8–40.5)

130.2 (118.9–140)

2,013

2.2 (1.9–2.6)

2.8 (2.4–3.3)

24 (20.5–31.9)

68.6 (58.6–80.9)

23.9 (12.5–37.3)

126 (112.5–136.7)

2,014

2.2 (1.8–2.6)

2.9 (2.6–3.5)

23.5 (20.2–29)

51.6 (43.9–60.1)

19.8 (9.4–32)

121.5 (105.6–136.7)

2,015

2.1 (1.7–2.6)

3.1 (2.7–3.7)

22.9 (19.8–27.2)

38.9 (33.7–44.4)

15.9 (7–25.3)

117.2 (99.8–137)

2,016

2.1 (1.7–2.6)

3.4 (2.9–4)

22.4 (19.4–26)

30 (27–34.4)

12.4 (5.3–18.2)

114.3 (96–137.5)

2,017

2.1 (1.7–2.6)

3.7 (3.2–4.3)

21.8 (18.9–25)

24.7 (20.8–28.6)

9.7 (4–13.8)

112.3 (95–138.2)

2,018

2.2 (1.8–2.6)

4.1 (3.5–4.8)

21.3 (18.6–24)

22.2 (17.9–25.9)

7.6 (3.1–11.7)

112.5 (96.9–138.8)

2,019

2.3 (1.9–2.6)

4.5 (3.9–5.3)

20.8 (18.3–23.1)

21.6 (17.6–25)

6.4 (2.3–10.2)

116.3 (102–139.3)

2,020

2.3 (2–2.7)

5.1 (4.4–5.8)

20.2 (18–22.3)

22.7 (19.5–25.8)

5.8 (1.8–9)

123 (108.1–140.2)

2,021

2.4 (2.1–2.8)

5.8 (5–6.4)

19.7 (17.7–21.6)

25.6 (22.6–28.6)

5.4 (1.3–8.2)

130.8 (115.1–146)

2,022

2.5 (2.2–2.9)

6.6 (5.9–7.2)

19.1 (17.3–21)

30 (27.1–34.2)

5.4 (1–8.1)

137.5 (121.6–155.8)

2,023

2.6 (2.3–3)

7.5 (6.8–8.2)

18.7 (16.9–20.5)

35.3 (31.4–40.8)

5.2 (0.8–8.3)

143.6 (129.2–165.7)

2,024

2.7 (2.4–3.1)

8.7 (7.7–9.6)

18.2 (16.3–20.1)

39.2 (34.7–43.6)

5 (0.6–8.4)

149.7 (134.2–168)

2,025

2.8 (2.4–3.3)

10 (8.7–11.4)

17.7 (15.5–20)

40.8 (35.1–46.6)

4.3 (0.4–9.1)

153.7 (136.4–173.8)