Methods
Breeding red-tailed tropicbirds were tagged on Round Island, Mauritius (19.8486° S,
57.7885° E), where breeding activity peaks between August and October (when > 25% of
nest sites are occupied). The lowest breeding activity occurs between January and April (<
5% of nests are occupied (unpublished results
29,30 ). During chick rearing, birds were
equipped with a Daily Diary tag (Wildbyte Technologies, Swansea University, UK) and a
GPS logger (GiPSy 5, Technosmart Europe, Guidonia-Montecelio, Italy) as detailed in Garde
et al. 25. The Daily Diary recorded acceleration and magnetic field strength, each in 3 axes
and at 40 and 13 Hz respectively. Barometric pressure and temperature were logged at 4 Hz,
and GPS location was recorded once per minute. Both loggers were placed in a zip-lock bag
and fixed to the back feathers using Tesa tape
31. The loggers, housing and tape weighed 27.7
g, representing < 3% of the average body mass (mean body mass for tagged birds was 826 g),
and 4.3% of the lowest body mass recorded during this study (650 g). Birds were weighed
and photographed to quantify wing area and loading following Pennycuick
10. Ethical
permission was granted by Swansea University AWERB, permit 040118/39.
Wind speed, direction, atmospheric pressure, relative humidity and temperature were
recorded every 5 minutes by a portable weather station (Kestrel 5500L, Kestrel instruments,
USA) mounted on a 5 m pole stationed at the highest point of Round Island (280 m ASL).
Wind records for 7 flights were interrupted due to battery failure (between 9
th and 20 th
February 2018). Here wind data were replaced by hourly wind records from Sir Seewoosagur
Ramgoolam International Airport in Mauritius (downloaded from
http://www.wunderground.com)
. Temperature, pressure, wind speed, wind direction and
relative humidity were synchronised with the GPS data and linearly interpolated to 1-minute
intervals.
Flight metrics
Flight was evident as periods with variable altitude and was categorised as flapping or non-
flapping flight using a simple acceleration threshold
25. Specifically, the Vectorial sum of the
Dynamic Body Acceleration (VeDBA) was calculated according to Wilson et al. 32, using
smoothed raw acceleration values over two seconds to derive the gravitational component.
VeDBA values were themselves smoothed over two seconds (sVeDBA) to produce a metric
that varied between high and low levels of activity. A threshold of
≥ 0.4 g was used to
identify flapping flight, which distinguished between flight types across individuals and
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seasons. The identification of flapping and gliding was undertaken in R Studio version
4.0.033.
Wingbeat frequency was used as a proxy for flight effort rather than DBA 34,35, as we
identified a difference in the stability of the accelerometer attachment between the two
seasons, which led to consistent differences in the amplitude of the acceleration signal 15.
Wingbeat frequency was robust to small changes in logger attachment and has been used to
estimate work rate in a range of studies (e.g. 34,35, though see 36). Individual wingbeats were
identified from peaks in the dynamic heave acceleration, smoothed over 3 events (0.075 s)
following Krishnan et al. 36. In brief, peaks were identified as the highest values in the heave
acceleration that occurred within five points of the positive to negative turning point in the
rate of change of the heave acceleration. Each segment between successive peaks was
counted as a wingbeat cycle, and the duration was used to calculate wingbeat frequency.
Frequencies < 4 Hz were considered erroneous for birds of this body mass
10 (potentially
resulting from manoeuvring or peak misidentification) and were therefore removed.
Flight altitude above sea level was calculated using the barometric pressure recorded by the
Daily Diary (4 Hz), corrected for daily changes in sea-level pressure (taken from
https://earth.nullschool.net/
). Pressure values from the tags were smoothed over 2 s and the
rate of change of altitude (Vz) was calculated over 1 second intervals. The air density at flight
altitude was estimated using the ideal gas law, using pressure measured by the Daily Diary
and the temperature and relative humidity recorded by the weather station.
The bird’s groundspeed ( V
g) was taken as the haversine distance between GPS fixes divided
by the time. The airspeed (V a) was estimated following Pennycuick 10, taking wind values
from the anemometer. The headwind and crosswind components (HWC and CWC) were
calculated as the two components of the wind acting on airspeed. A positive HWC indicates a
headwind and a negative HWC corresponds to a tailwind.
Red-tailed tropicbirds are surface feeders
37 with regurgitates from birds on Round Island
being mostly made up of flying fish. Prey pursuits were evident as rapid losses of altitude,
temporary cessation of flapping flight and characteristic changes in the acceleration data
indicative of manoeuvring (Fig. S2). These events were identified manually using custom-
written animal movement analysis software DDMT (Wildbyte Technologies,
http://wildbytetechnologies.com/software.html
). We assumed that these represented most
prey-encounters as there were no other obvious periods with bursts of acceleration and birds
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only ever dipped underwater for periods < 1.5 seconds, with these brief submersions usually
occurring at the end of aerial pursuits.
Statistical analysis
Seasonal differences in environmental and foraging parameters were tested as follows.
Wilcoxon tests were used to test for differences in the body mass and wing area of tagged
tropicbirds, as well as wind speed and temperature. Student’s t-tests were used to compare air
density and chick age. Wind speed, temperature and air density were averaged over all flights
per day in these tests to avoid pseudo-replication. Simple LME models were used to test
whether total distance covered, wingbeat frequency, prey encounter rate and foraging
efficiency varied between the two seasons, with individual as a random factor.
Birds vary their airspeed in relation to the wind, increasing their airspeed in headwinds and
reducing it in tailwinds
20. We therefore expected that we would be able to use either airspeed
or wind in our model of wingbeat frequency and ran an LME to assess how much variation in
airspeed was explained by wind and air density (birds are also expected to increase their
airspeed with decreasing air density)
7,38. The model included the fixed effects of headwind
and crosswind components, as well as wind strength, to test whether the estimated head and
crosswind components captured all the variation due to changing wind conditions. Flight
altitude was also included in the model to account for potential changes in currency (and
associated speed selection) between relatively high and low altitude flight. This model was
constrained to periods of level flapping flight (taken as periods where -0.2 < V
z 0.3 g), to control for changes in airspeed that occur in relation to
climbing and descending flight 39. Individual bird ID was included as a random factor nested
within foraging trip to account for unmeasured differences between days and individuals. We
tested for collinearity by calculating the Variance Inflation Factors (VIF) of every fixed effect
using the package “performance”
40. An autocorrelation structure of order 1 was also
integrated to the model to account for the high level of autocorrelation in the GPS data (lag =
40).
Finally, we used an LME model to examine the factors causing the seasonal difference in
wingbeat frequency. Here, we averaged values of airspeed, air density and flight altitude
between successive prey pursuits to distinguish the effects of increasing body mass due to
foraging success, from the effects of the physical environment. Only foraging trips with 5- 15
pursuits and inter-pursuit intervals > 1 minute were included, resulting in 345 segments
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recorded over 48 trips from 41 birds. One outlier segment with a mean altitude > 250 m was
excluded, as all other segments had a mean altitude < 150 m. The number of pursuits was
included as a fixed effect in interaction with season, to identify any seasonal differences in
foraging success. The presence of airspeed in the model accounted for the expected effects of
the wind on the wingbeat frequency. Air density and altitude were both included in the model
to enable us to distinguish between the effects of changing flight altitude and seasonally
changing temperatures. “Individual” was used as random factor nested within “foraging trip”.
Statistical analyses were carried out using R Studio, using the packages nlme (Pinheiro et al.
41, version 3.1-151) and MuMIn (Barton and Barton 42, version 1.43.17).
Estimation of density altitude
The following equations describe temperature, pressure and density of the air in the
international standard atmosphere (ISA) within the troposphere, which extends up to 11 km
altitude:
/g1846/g3404 /g1846 /g2868 /g3398/g1838 /g1834 ( 1 )
/g1842/g3404/g1842 /g2868 /g46721 /g3398
/g3013/g3009
/g3021 /g3116
/g4673
/g3282/g3262
/g3267/g3261
( 2 )
/g1830/g3404
/g3017/g3014
/g3019/g3021/g2869/g2868/g2868/g2868 ( 3 )
where T = ISA temperature in deg K
P = ISA pressure in Pa
D = ISA density in kg/m3
H = ISA geopotential altitude in km
These can be rearranged to express geopotential altitude as a function of density:
/g1834/g3404 /g4672
/g3021 /g3116
/g3013 /g4673/g4680 1/g3398/g4674
/g2869/g2868/g2868/g2868/g3019/g3021 /g3116/g3005
/g3014/g3017 /g3116
/g4675
/g3261/g3267
/g3282/g3116/g3262/g3127/g3261/g3267/g4681 (4)
This can be simplified to the following when ISA constants are used:
/g1834 /g3404 44.3308 /g3398 42.2665/g1830 /g2868./g2870/g2871/g2872/g2877/g2874/g2877 (5)
where H = geopotential altitude in kilometres.
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Figure 1.
Figure 1 . (a) Foraging movements of red-tailed tropicbirds from Round Island (indicated
with a black star, lying to the north of mainland Mauritius). (b) The frequency of flight power
values estimated across the red-tailed tropicbird distribution during the Austral summer
(December, January, February, DJF) and winter (June, July, August, JJA). (c) Spatial
variation in flight power as a function of regional variation in air density within the red-
tailed tropicbird range. The power required to fly was estimated using apft
17, using the
morphological measurements of a red-tailed tropicbird of average mass from Round Island
flying at its maximum range speed (V
mr), in varying air densities. The breeding distribution is
taken from BirdLife International (http://datazone.birdlife.org/species/requestdis). Monthly
mean values of air density were estimated from ERA5 for 2001-2020
(https://cds.climate.copernicus.eu/cdsapp#!/dataset/reanalysis-era5-single-levels-monthly-
means?tab=overview)
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Figure 2.
Figure 2. The effective altitudes, hereafter “density altitudes” (top two panels), experienced
by any bird flying at sea level in two seasons (December, January and February, left panel,
and June, July and August, right panel). Density altitude is the altitude corresponding to a
given air density when compared to the reference density at sea level for the international
standard atmosphere (ISA) (1.255 kg m
-3) (see SI). The relative frequencies of the density
altitudes are shown below the maps for each latitudinal zone. Tropical and temperate
latitudes have modal peaks around 700 m and -200 m respectively.
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