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DOI: 10.1111/j.1366-9516.2006.00284.x © 2006 The Authors
502
Journal compilation © 2006 Blackwell Publishing Ltd www.blackwellpublishing.com/ddi
Diversity and Distributions, (Diversity Distrib.)
(2006)
12
, 502–510
BIODIVERSITYRESEARCH
ABSTRACT
We examined the influence of ‘seasonal fine-tuning’ of climatic variables on the per-formance of bioclimatic envelope models of migrating birds. Using climate data andnational bird atlas data from a 10
×
10 km uniform grid system in Finland, we testedwhether the replacement of one ‘baseline’ set of variables including summer (June–August) temperature and precipitation variables with climate variables tailored(‘fine-tuned’) for each species individually improved the bird-climate models. Thefine-tuning was conducted on the basis of time of arrival and early breeding of thespecies. Two generalized additive models (GAMs) were constructed for each of the63 bird species studied, employing (1) the baseline climate variables and (2) the fine-tuned climate variables. Model performance was measured as explanatory power(deviance change) and predictive power (area under the curve; AUC) statisticsderived from cross-validation. Fine-tuned climate variables provided, in many cases,statistically significantly improved model performance compared to using the samebaseline set of variables for all the species. Model improvements mainly concernedbird species arriving and starting their breeding in May–June. We conclude that theuse of the fine-tuned climate variables tailored for each species individually on thebasis of their arrival and critical breeding periods can provide important benefits forbioclimatic modelling.
Keywords
Bird atlas, boreal regions, distribution, model accuracy, species-climate model.
INTRODUCTION
Recent studies suggest that the ongoing climate change has
already caused changes in bird species phenology, migration and
distribution patterns (Thomas & Lennon, 1999; Both & Visser,
2001; Ahola
et al
., 2004; Brommer, 2004; Crick, 2004). Simula-
tions of the impacts of climate change on species distributions
are often based on bioclimatic envelope models (e.g. Berry
et al
.,
2002; Thuiller, 2003). These models relate present species
distributions to selected aspects of present climate and fit the
derived models into different climate change scenarios to predict
the potential changes of species’ geographical distributions
(Huntley, 1995; Pearson & Dawson, 2003; Thuiller, 2003). The
approach has been applied to birds by, e.g. Berry
et al
. (2001),
Peterson
et al
. (2002), Peterson (2003) and Araújo
et al
. (2005a,b).
A crucial factor in developing species distribution models,
including bioclimatic envelope models, is the use of the most
appropriate predictor variables possible. As argued by Austin
(2002), modellers should, wherever possible, use direct and more
proximal (e.g. rainfall) rather than indirect or distal predictors
(e.g. altitude, latitude). However, the demands for careful
selection of variables are especially high in bioclimatic models.
This is because these models and their projections can have an
important role in conservation planning and political debates.
Thus, there are high demands on their accuracy and plausibility
(Araújo
et al
., 2005a). Recent research has highlighted the
fact that bioclimatic models can be vulnerable to a number of
uncertainties (Pearson & Dawson, 2003; Hampe, 2004; Araújo
et al
., 2005b; Luoto
et al
., 2005), e.g. critical issues in model
building and the selection of climatic variables for a given study
(Kadmon
et al
., 2003; Thuiller
et al
., 2004; Thuiller, 2004; Araújo
et al
., 2005a; Beaumont
et al
., 2005). In the case of migratory
birds, one potential source of uncertainty is the delineation of
the climatic variables used in modelling bird species responses.
Hitherto, very little attention has been paid to the selection of
as accurate climatic variables as possible in the migratory
Finnish Environment Institute, Research
Department, Research Programme for
Biodiversity, Helsinki, Finland
*Correspondence: R. K. Heikkinen, Finnish Environment Institute, Research Department, Research Programme for Biodiversity, P.O. Box 140, FIN-00251 Helsinki, Finland. Tel.: + 358 9 40300249; fax: + 358 9 40300290; E-mail: [email protected]
Blackwell Publishing Ltd
Does seasonal fine-tuning of climatic variables improve the performance of bioclimatic envelope models for migratory birds?
R. K. Heikkinen*, M. Luoto and R. Virkkala
Fine-tuning of bird-climate models
© 2006 The Authors
Diversity and Distributions
,
12
, 502–510, Journal compilation © 2006 Blackwell Publishing Ltd
503
birds–climate impacts models. Such attention can be particularly
important at high latitudes (e.g. North Europe), from where
several bird species migrate south for the winter (Newton &
Dale, 1996). The breeding ranges of these species may be largely
determined by the climate conditions prevailing at the time of
their arrival, courtship and breeding (Virkkala, 1991; Huntley,
1995; Lennon
et al
., 2000).
Climate variables used in bird–climate models have varied
considerably. Some studies have employed only mean annual
precipitation and temperature values (e.g. Peterson, 2003;
Seoane
et al
., 2003). By contrast, Araújo
et al
., (2005a) used, for
example, temperature of the coldest and warmest month and
July–September precipitation in addition to annual values.
Some other multi-species studies have focused more on the
relationships between birds and climate conditions of spring or
early summer, i.e. precipitation and temperature of April–June
(Forsman & Mönkkönen, 2003; Lemoine & Böhning-Gaese,
2003; Virkkala
et al
., 2005) or May–July (Lennon
et al
., 2000;
Berry
et al
., 2001). However, it has rarely been examined whether
applying climate variables tailored (‘seasonally fine-tuned’)
separately for each of the bird species individually instead of
using one common set of climate variables for all the studied
species would increase model performance (cf. Huntley, 1995).
This paucity of bird–climate modelling studies considering the
fine-tuning of variables is surprising because autecological
studies have indicated that the climate conditions during the
period of courtship and the early weeks of breeding can
markedly influence the occupancy patterns and breeding success
of birds (Redpath
et al
., 2002; Rodríguez & Bustamante, 2003;
Jovani & Tella, 2004). Consequently, many multi-species model-
ling studies that have included a large number of migratory bird
species (e.g. Brotons
et al
., 2004; Araújo
et al
., 2005b) may have
been exposed to a possible mismatch of climate variables and
critical periods in breeding, and to lowered model accuracy for
these species.
In this study, we used generalized additive models (GAM) and
distribution data of 63 migratory bird species in Finland at the
resolution of 10
×
10 km to examine whether the seasonal
fine-tuning of climate variables based on the arrival and early
breeding periods of the studied species improves the performance
of bird–climate models. Specifically, we addressed the following
questions: (1) Does the replacement of baseline summer (June–
August) climate variables with variables tailored for each species
individually significantly improve the accuracy of the models?
(2) Are the possible model improvements related to the time of
arrival and breeding of the studied bird species?
METHODS
Study area
Finland covers an area of
c
. 338,000 km
2
in northern Europe
between latitudes 59
°
30
′
and 70
°
N. The climate shows char-
acteristics of both an oceanic and a continental climate, the
continentality growing inland and eastwards (Tuhkanen, 1984).
The majority of the country has a boreal climate, with a decrease
in rainfall and temperature from the south-western hemiboreal
zone (mean annual temperature
c
. 5
°
C and mean annual precipi-
tation 600–700 mm) to the subarctic region in northernmost
Finland (
−
2
°
C and 400 mm). Biogeographically, Finland is
located mainly in the boreal coniferous vegetation zone, and the
landscape is largely dominated by forests and mires.
Bird data
The studied 63 land bird species bred and/or foraged in the
main terrestrial habitats: 19 species occurred primarily in forests,
17 species in agricultural and bushy habitats, 13 species in
mires, 9 species in marshes and coastal wetlands and 5 species
in mountain heaths (see Appendix S1 in Supplementary
material). Nomenclature of the species follows Dickinson (2003).
The species were assigned to three groups according to their
average arrival–early breeding period: those arriving and having
their early breeding period in (1) March–April (2) April–May, or
(3) May–June (see Appendix S1). This classification was based
on a literature survey of the key publications of the migratory
periods of bird species in Finland (e.g. Hildén
et al
., 1979;
Pöyhönen, 1995).
The information on the distribution of species and the level of
survey activity was extracted from the second bird atlas survey in
Finland, which was carried out in 1986–1989 and included 3800
squares of 10
×
10 km (Väisänen
et al
., 1998). Recorders and
organizers of the survey graded the survey activity in each square
according to six categories: 0 = no observations, 1 = occasional
observations, 2 = fair survey, 3 = satisfactory survey of the
square, 4 = well surveyed and 5 = thoroughly surveyed square
(Väisänen
et al
., 1998). We used only squares with survey
activities of 2–5 in our analysis. Consequently, the data used in the
analyses consisted of 2861 squares. Väisänen
et al
. (1998) listed
the breeding status of bird species recorded in each of the grid
squares in four classes: 0 = not found, 1 = breeding possible,
2 = breeding probable and 3 = confirmed breeding. For the
analysis of this study, we combined classes 1, 2 and 3 as a species-
present variable.
Climate data
Climate data produced by the Finnish Meteorological Institute,
using the same 10
×
10 km grid system, were employed as pre-
dictors of the bird distribution data (Venäläinen & Heikinheimo,
2002). The climate data included mean values for the period
1985–1989 for all climatic variables. Because we focused on
analysing the impacts of fine-tuning on the performance of
bird–climate models, we used a limited number of variables.
The baseline set of predictors simulated the commonly used
approach of using one set of explanatory variables for all species.
It included three variables: mean temperature of the coldest
month (MTCO), mean summer temperature (defined as June–
August; TEMPSUM), and mean summer precipitation (June–
August; PRESUM). For the fine-tuning analysis we calculated the
mean values for three pairs of months: mean temperature of
March–April (TEMMA), April–May (TEMAM) and May–June
R. K. Heikkinen
et al.
© 2006 The Authors
504
Diversity and Distributions
,
12
, 502–510, Journal compilation © 2006 Blackwell Publishing Ltd
(TEMMJ), and mean precipitation of March–April (PREMA),
April–May (PREAM) and May–June (PREMJ). MTCO was
included to indicate the general harshness of the environmental
conditions in each grid square.
Model calibration
Generalized additive models were developed using
(Generalized Regression Analysis and Spatial Prediction)
(Lehmann
et al
., 2003) in S-Plus (version 6.1 for Windows,
Insightful Corp.). All the GAMs were built using a binomial
distribution of error and a logistic link function, and a stepwise
selection procedure to select important explanatory variables
and the level of complexity of the response shapes of the various
species to each variable. A starting model including all continuous
predictors smoothed with 4 degrees of freedom was fitted first.
Next, the stepwise
procedure proceeded in a loop that
aimed to eliminate one variable at a time from the full model. At
each step, the least significant variable was dropped from the
model or converted to a linear form, after which the loop
proceeded with the remaining variables (see Lehmann
et al
.,
2003). The final models for different species may thus include
different numbers of predictors with either 1 or 4 degrees of
freedom for the spline smoother. The variable dropping or
conversion to linear form was tested in the first set of GAMs
using Akaike’s Information Criterion (AIC) (Akaike, 1974).
The modelling procedure included building two GAMs for
each species. In the first set of GAMs (‘baseline GAMs’), the three
baseline climate variables (MTCO, TEMPSUM, PRESUM) were
used as the three explanatory variables. In the second set of
GAMs (‘fine-tuned GAMs’), mean summer temperature was
replaced by one of the fine-tuned temperature variables
(TEMMA, TEMAM, TEMMJ) and mean summer precipitation
by one of the precipitation variables (PREMA, PREAM, PREMJ),
based on the information on the average arrival-early breeding
periods of the studied species (Appendix S1). In all the models,
the three climate predictors included were subjected to the
stepwise variable selection process in order to develop
parsimonious models, as described in the previous paragraph.
Model evaluation
The models were evaluated in two ways. First, the explained
deviance in each model (i.e. the ratio of explained deviance vs.
the total deviance) was investigated. This was regarded as the
‘explanatory’ power of the model. Second, we examined the
cross-validation statistics in each model (the ‘predictive’ power of
the model). Cross-validation was made with four spatially
random subsets of the entire data set. Each subset was dropped
from the model, the model was recalculated and predictions
were made for the omitted data points (see Lehmann
et al
.,
2003). Predictive power was then measured using the area under
the curve (AUC) of a receiver operating characteristic (ROC)
plot (Fielding & Bell, 1997).
Model validation using cross-validation based on spatially
random sets of grid squares may be vulnerable to the effects of
spatial autocorrelation in the predictor and response variables
(e.g. Legendre, 1993; Koenig, 1999). Cross-validation based on
random regions (Peterson, 2001) or random blocks of, e.g.
100
×
100 km (cf. Augustin
et al
., 2001) may circumvent
autocorrelation problems better but they may cause other kind
of difficulties for validation. For example, use of large random
regions may lead to loss of information because not all species
necessarily occur in acceptable numbers in both calibration and
evaluation data sets (see Peterson, 2001). Random blocks of,
e.g. 100
×
100 in in size would work slightly better in this respect.
However, as several of the studied species have very narrow dis-
tributions in Finland, the model validation using random blocks
would also result in losing species information. Validation using
both random regions and random blocks may be vulnerable to
the risks of comparing different sampling strategies or field
survey activities instead of evaluating a model (Lehmann
et al
.,
2003).
There is a plethora of techniques available for examining
spatial autocorrelation structure and its impacts (e.g. Legendre,
1993; Lichstein
et al
., 2002; Diniz-Filho
et al
., 2003). However,
we do not examine spatial autocorrelation in our data with such
techniques here, mainly because (1) in some biogeographical
study settings similar to our work, autocorrelation in species data
have been shown to be largely accounted for by the similarly auto-
correlated climate predictors (Diniz-Filho
et al
., 2003), and (2),
our climate variables are rather closely correlated (see Table 1)
and thus we presume that potential autocorrelation would have
a broadly equal impact on the validation of the baseline and on
fine-tuned GAMs, and would not alter our comparative results.
However, instead of applying more sophisticated techniques
to examine autocorrelation issues, we use a simple ad hoc, but
prudent, course of action to take its potential impacts into
account in the modelling. One of the core impacts of spatial
autocorrelation is that type I errors may be inflated, i.e. coeffi-
cients declared to be significantly different from zero when in
fact they are not (Legendre, 1993). A simple means to take this
into account is to reduce the probability levels in model inference
tests (Koenig, 1999; Guisan & Thuiller, 2005). Consequently, we
re-ran all our GAMs using the fourfold cross-validation process
Table 1 Correlations (Spearman’s rho) between the two ‘baseline’ summer (June–August) climate variables and three ‘fine-tuned’ climate variables (March–April; April–May; May–June)
Summer temperature Summer precipitation
Temperature
March–April 0.899*** —
April–May 0.939*** —
May–June 0.947*** —
Precipitation
March–April — 0.603***
April–May — 0.661***
May–June — 0.521***
***P < 0.001.
Fine-tuning of bird-climate models
© 2006 The Authors
Diversity and Distributions
,
12
, 502–510, Journal compilation © 2006 Blackwell Publishing Ltd
505
but accompanied with
F
-tests using a stringent probability limit
(0.001) for the selection of the predictors. The results of the
AIC-based and
F
-test–based GAMs were then compared.
To examine the differences in the explanatory and predictive
power of the models, we compared the explained deviance
and AUC values from the baseline GAMs vs. fine-tuned GAMs
for each species. Because deviance and AUC data were not sig-
nificantly different from normal distribution (Kolmogorov-
Smirnov tests,
P
> 0.05), we used paired
t
-test for measuring the
significance between the baseline and fine-tuned models.
Because we expected a priori that fine-tuned climatic variables
would improve the model fitting, we used one-tailed
t
-tests in all
analyses. Paired one-tailed
t
-tests were conducted first for all the
63 studied species simultaneously, and then for the early and mid
(March–April and April–May) arriving bird species (‘early and
mid arrivers’;
n
= 29) vs. late spring (May–June) arriving species
(‘late arrivers’;
n
= 34) separately. The early and mid arrivers
were lumped in this analysis because of the low number of
species (
n
= 6) included in the first group.
As an example, we produced projected future distributions for
selected study species based on both the derived baseline and the
fine-tuned GAMs and using the climate data obtained from the
HadCM3 general circulation model (GCM) under the business-as-
might-be-usual (BAMBU) scenario A2, compiled by the EC FP6
Integrated Project ALARM (http://www.alarmproject.net). This
was carried out to examine whether the observed differences
in the predicted current distributions from the baseline and
fine-tuned models increase when the models are employed to
produce predictions of future distributions.
RESULTS
The summer temperature and the three fine-tuned temperature
variables were highly correlated with each other, whereas the
correlations between precipitation variables were moderate
(Table 1). Concurring with our a priori expectations, the explan-
atory power of fine-tuned models (model selection using AIC)
was on average significantly higher (mean percent of deviance
explained = 35.1%) than that of baseline models (mean = 34.5%)
(paired one-tailed
t
-test; d.f. = 62;
t
=
−
2.135;
P
= 0.018). In
addition, the predictive power (AUC) of the fine-tuned GAMs
(mean = 0.887) was slightly but statistically significantly higher
than that of the baseline GAMs (mean = 0.861) (paired one-
tailed
t
-test;
t
=
−
1.948;
P
= 0.028).
Separate analysis of the explanatory and predictive powers of
early mid and late arrivers revealed that the differences between
the performance of baseline and fine-tuned AIC-based GAMs
was caused by the models for May–June arrivers. Both the
deviance and AUC values were statistically significantly higher in
late arrivers models using fine-tuned climate variables than in
the baseline GAMs (Table 2). Moreover, in the models for
late arrivers there was a clear general trend towards fine-tuned
models providing higher performance (deviance change, 24
vs. 10 species; AUC, 22 vs. 8 species).
The results of the GAMs based on model selection using the
F
-
test and a probability level of 0.001 (Appendix S2 in Supplementary
material) were very similar to those of AIC-based GAMs. Thus,
correcting the model inferences for the potential autocorrelation
effects simply by reducing the probability levels did not alter our
results, and in the remaining part of the paper we will focus on
AIC-based modelling results.
The set of species for which the fine-tuning resulted in the
highest increase in model performance included birds from dif-
ferent taxonomical and habitat type groups, including turtle
dove
Streptopelia turtur
, arctic warbler
Phylloscopus borealis
,
hawfinch
Coccotraustes coccotraustes
, ring ouzel
Turdus torquata
,
grey heron
Ardea cinerea
, moorhen
Gallinula chloropus
and
black-tailed godwit
Limosa limosa
. The highest (24%) increase in
the predictive power was in the case of the black-tailed godwit.
As an example, the predicted distributions are presented for the
grey heron and the arctic warbler (Fig. 1). The overall pattern
of predicted probability of occurrence for the two species did
not vary greatly between the baseline and fine-tuned GAMs.
However, there were clear regional spatial differences in the
model accuracy. The fine-tuned models predicted better, e.g. the
northernmost occurrences of the grey heron and certain agglom-
erations of occurrences of both species along the eastern border
of the country.
Figure 2 shows the predicted future distributions for four
species based on fitting the derived species-specific baseline and
fine-tuned GAMs in the climate data obtained from the
HadCM3 GCM under the BAMBU scenario A2. The projected
distributions are, in the case of the arctic warbler, the same (both
models predict that a suitable climate for the species will not
exist in Finland in the future). In the case of the red-breasted
flycatcher
Ficedula parva
the differences are relatively small.
Table 2 Mean (± standard error) values of explained deviance (‘explanatory power’) and AUC (‘predictive power’) of the distribution models for (a) land bird species arriving in March–April and April–May (n = 29) and (b) arriving in May–June (n = 34). The models employ three ‘baseline’ climate variables (mean temperature of the coldest month, mean June–August temperature, mean June–August precipitation) or three ‘fine-tuned’ climate variables (mean temperature of the coldest month, mean temperature and mean precipitation of March–April/April–May/May–June, the latter two selected on the basis of species-specific arrival-early breeding period). Statistical tests by paired one-tailed t-test; AUC derived from fourfold cross-validation test; ranks: negative/positive/tied (negative rank = fine-tuned model < baseline model; positive rank = fine-tuned model > baseline model)
Species
group
Baseline
climate
variables
Fine-tuned
climate
variables t P Ranks
(a) Early mid arrivers
Deviance 0.319 ± 0.028 0.326 ± 0.026 −1.117 0.137 12/17/0
AUC 0.844 ± 0.014 0.852 ± 0.011 −1.258 0.109 13/14/2
(b) Late arrivers
Deviance 0.367 ± 0.026 0.373 ± 0.026 −2.422 0.011 10/24/0
AUC 0.876 ± 0.010 0.880 ± 0.010 −3.171 0.002 8/22/4
R. K. Heikkinen
et al.
© 2006 The Authors
506
Diversity and Distributions
,
12
, 502–510, Journal compilation © 2006 Blackwell Publishing Ltd
Figure 1 Recorded and projected distributions of two species: (a) recorded occurrence of the grey heron in grid squares of 10 × 10 km in 1986–1989, and probability of occurrence of the species based on (b) the ‘baseline’ bioclimatic envelope model, and on (c) the ‘fine-tuned’ bioclimatic model; (d) recorded occurrence of the arctic warbler in 1986–1989, and probability of occurrence of the species based on (e) the ‘baseline’ bioclimatic envelope model, and on (f) the ‘fine-tuned’ bioclimatic model. Probability is shown on a three-level scale. D2 = percentage of explained deviance; AUC = the area under the curve of a receiver operating characteristic (ROC) plot.
Fine-tuning of bird-climate models
© 2006 The Authors
Diversity and Distributions
,
12
, 502–510, Journal compilation © 2006 Blackwell Publishing Ltd
507
However, the projections for the grey heron and the turtle dove
show that the slight differences in the predicted current distribu-
tions may be more important when the models are fitted to the
climate scenarios. The difference in the AUC between the baseline
and fine-tuned GAMs was greatest in the case of the grey heron
(Appendix S1), which also showed the greatest difference in the
projected future distribution between the two models.
DISCUSSION
A number of bioclimatic envelope modelling studies have
employed multi-species simulations based on one set of climate
variables for all the studied species (e.g. Thuiller, 2003; Brotons
et al., 2004; Araújo et al., 2005a, b), although the variables
included have varied between the studies. For sedentary organ-
isms, especially plants, this approach may work well. Variables
such as mean annual temperature and precipitation, minimum
temperature of the coldest month, growing degree days and
moisture availability can have strong links with the physiology
and growth of plants (Huntley et al., 1995). The distributions
and densities of resident bird species may also be adequately
modelled using a combination of winter and summer climate
variables or mean annual variables (Huntley, 1995; Forsman &
Mönkkönen, 2003; Seoane et al., 2003).
However, more mobile species such as migratory birds pose
challenges for developing accurate bioclimatic models. As Huntley
(1995) argued, it is probable that one set of climate variables will
not be applicable to all birds in the manner that one set of key
variables (e.g. growing degree days, mean temperature of the
coldest month and moisture availability) can be applied to a wide
range of terrestrial plant species. Our results suggested that the
explanatory and predictive power of the species–climate models
especially for birds arriving and breeding in May–June in Finland
can be enhanced by replacing the summer climate variables with
fine-tuned climate variables. Although the absolute increases
in the amount of explained deviance and cross-validation AUC
values were generally small, they were rather systematic and
statistically significant. We consider these differences important
for three reasons. First, as the fine-tuned climate variables always
provided better or equally good model performance than
the baseline summer variables, we see no reason not to use the
ecologically more reasonable fine-tuned variables in modelling
Figure 2 Projected future distributions of four bird species in Finland based on models calibrated with climate and species data from the 1980s and fitted to the climate variable data obtained from the HadCM3 GCM under the BAMBU scenario A2 for the year 2050: the occurrence of (a) the grey heron (Ardea cinerea) based on the ‘baseline’ GAM and (b) the ‘fine-tuned’ GAM; (c) the turtle dove (Streptopelia turtur) based on the baseline GAM and (d) the fine-tuned GAM; (e) the arctic warbler (Phylloscopus borealis) based on the baseline GAM and (f) the fine-tuned GAM; and (g) the red-breasted flycatcher (Ficedula parva) based on the baseline GAM and (h) the fine-tuned GAM. Black dots represent the 10-km grid squares modelled as suitable for the species (projected presence) and unmarked were areas modelled as not suitable (projected absence). To determine the probability thresholds at which the predicted values for species occupancy are optimally classified as absence or presence values, we used prevalence of the species as the probability level as suggested by Liu et al. (2005).
R. K. Heikkinen et al.
© 2006 The Authors508 Diversity and Distributions, 12, 502–510, Journal compilation © 2006 Blackwell Publishing Ltd
the species studied here. In other words, the use of fine-tuned
predictors should inherently improve the mechanistic basis of
the bioclimatic envelope models for migratory birds. Second,
particularly in the results for the late arrivers, there was a clear
trend of the fine-tuned GAMs outcompeting the baseline GAMs.
Third, recent studies have suggested that even slight differences
between current predictions from different bioclimatic models
can be exacerbated when the models are used for simulating
future distributions (Thuiller, 2003; Araújo et al., 2005b). However,
it should be noted that in the work of Thuiller (2003) and Araújo
et al. (2005b), the differences between the simulated future
distributions were caused by the differences between modelling
methods. One of the lessons learned from the results of our study
is that a priori selection of the climate predictors can also result
in intensified differences in the future projections of species
distributions and represents another important source of
uncertainty in bioclimatic models (cf. Heikkinen et al. in press).
The reason why the increases in the model performances
between baseline and fine-tuned models were not greater is
probably the result of the considerably high correlations between
the mean spring and summer temperatures for the period of
1985–1989 in Finland (Table 1; see also Järvinen, 1989). Summer
climate variables can thus act as statistically reasonable, but
ecologically imprecise, surrogate predictors of migratory bird
species distributions. Moreover, it is probable that the impact of
climatically deviating years (e.g. exceptionally warm or cold
springs) on the occupancy and density patterns of migratory
birds in boreal regions (see Järvinen, 1989; Virkkala, 1991; Ahola
et al., 2004) may be ‘lost’ in the mean climate values of longer-
term data, even though their influence in the species distributions
may be visible in the atlas maps.
Our results have some general implications for the bioclimatic
envelope modelling of birds. First, if one combination of climate
variables is used in modelling studies including migratory bird
species, it is intuitively more appropriate to use the mean
temperature or precipitation of periods such as May–July (e.g.
Lennon et al., 2000; Lemoine & Böhning-Gaese, 2003) than
variables extending to August–September (cf. Brotons et al.,
2004). The potential dangers of the mismatch in migratory bird–
climate models in boreal regions are most apparent in the case of
waders, such as whimbrel Numenius phaeopus and greenshank
Tringa nebularia studied here, which finish their breeding and the
adult birds start their ‘autumn’ migration already in June–July. In
the modelling of such species, late summer climate conditions
have a smaller role than spring and early summer climate.
However, this does not necessarily mean that the climate of all
other months than the migratory or residence periods is
completely irrelevant for the distribution and occupancy rates of
migratory birds. For example, lack of winter rains or severe cold
periods in winter may result in limited vegetation growth or food
(e.g. insects) availability and thus lower the suitability of habitats
for birds in the following summer (cf. Rodríguez & Bustamante,
2003). However, the relative explanatory power of migratory-
residence period climate vs. the climate conditions of the rest of
the year has rarely been examined in the same multiple regression
settings. The few results available, including those of Lennon
et al. (2000), have suggested that the single most powerful
explanatory variable for individual species distributions is May–
July temperature.
Second, we argue that distribution modelling of migratory
birds would benefit from using climate variables tailored for each
species individually. Recent autecological studies on migratory
birds have shown that particularly the climate conditions during
the arrival, courtship and early breeding period affect the
occupancy patterns and breeding success of birds (Redpath et al.,
2002; Rodríguez & Bustamante, 2003; Jovani & Tella, 2004). In a
detailed study of the lesser kestrel Falco naumanni (Fleischer,
1758), Rodríguez & Bustamante (2003) showed that the
occupancy rates among the colonies were best explained by the
temperature and rainfall during the courtship period in April–
May, the rainfall in spring being also a key determinant of the
nest success rate and the mean number of chicks per nest. Incor-
porating species-specific knowledge of the critical climate factors
from autecological studies into the multi-species bioclimatic
modelling exercises would decrease the uncertainty of the
models stemming from the possibly loosely delimited climate
variables, and yield information on the response of the species to
climate in different parts of its geographical range (cf. Redpath
et al., 2002).
In our results, the application of fine-tuned variables
improved significantly the overall model performance of the
studied species and especially the models of May–June arrivers.
This may be related to the phenomenon discussed by Kalela
(1952) who argued that migratory birds that overwinter in the
tropics and arrive in the breeding regions in the late spring can
respond to increased spring temperatures by a prolongation of
migration and a rapid occupation of new areas. Such species
include insectivorous birds such as grasshopper warbler
Locustella naevia and reed warbler Acrocephalus dumetorum,
which showed a rapid spread of distribution in the warm periods
in the 1930s in Finland. Moreover, Väisänen et al. (1998) argued
that the expansion of, e.g. the river warbler Locustella fluviatilis in
the 1980s and 1990s can be explained by prolonged migration as
a result of the warming of late spring. However, Kalela linked the
prolongation of migration-improved spring climate relation-
ships also to certain short-distance migrants that arrive earlier in
spring to northern Europe, such as lapwing Vanellus vanellus and
moorhen G. chloropus. Similarly, in our results, the group of
species with the greatest improvements in model performance
did not form a uniform group consisting of long-distance tropical
migrants.
We conclude that the use of the fine-tuned climate variables
tailored for each species individually on the basis of their arrival
and critical breeding periods can provide important benefits. In
other words, researchers can improve the accuracy and plausibility
of the migratory birds–climate models by applying fine-tuned
climate variables instead of the general approach used in multi-
species modelling studies (i.e. applying one set of predictors for
all species). Taking the species differences in arrival and breeding
periods into account is particularly essential at high latitudes, e.g.
North Europe, where the proportion of the species migrating for
the winter can be 50% or more (Newton & Dale, 1996). Overall,
Fine-tuning of bird-climate models
© 2006 The AuthorsDiversity and Distributions, 12, 502–510, Journal compilation © 2006 Blackwell Publishing Ltd 509
it is evident that bioclimatic modelling of migratory birds poses
greater challenges for investigators than developing useful
models for more sedentary organisms.
ACKNOWLEDGEMENTS
Niko Leikola and Stefan Fronzek helped in aggregating the
climate and bird data. The comments by the four referees helped
greatly in improving our paper. This research was funded by the
EC FP6 Integrated Project ALARM (GOCE-CT-2003-506675).
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SUPPLEMENTARY MATERIAL
The following material is available online at
www.blackwell-synergy.com/loi/ddi
Appendix S1. List of 63 Finnish bird species used in the migratory
birds-climate modelling (GAMs), based on two different sets of
climate variables: (1) one common ‘baseline’ set of variables
(mean temperature of the coldest month, mean June–August
temperature, mean June–August precipitation), and (2) three
‘fine-tuned’ climate variables (mean temperature of the coldest
month, mean temperature and mean precipitation of March–
April/April–May/May–June.
Appendix S2. Mean values of explained deviance and the area
under the curve (AUC) of the F-test-based distribution models
for (1) land bird species arriving in March–April and April–May
(n = 29) and (2) arriving in May–June (n = 34).