Turbulence explains the accelerations of an eagle in natural flight

TL;DR

This study demonstrates that turbulence significantly influences eagle flight accelerations, with measurable effects on their movement patterns, which can inform understanding of avian energetics and atmospheric conditions.

Contribution

It provides the first quantitative link between turbulence and eagle accelerations, showing a linear interaction across relevant timescales in natural flight.

Findings

Eagle accelerations correlate with turbulence intensity.

Accelerations can be several times stronger than gravity due to turbulence.

Turbulence impacts eagle behavior at timescales of 0.5 to 10 seconds.

Abstract

Turbulent winds and gusts fluctuate on a wide range of timescales from milliseconds to minutes and longer, a range that overlaps the timescales of avian flight behavior, yet the importance of turbulence to avian behavior is unclear. By combining wind speed data with the measured accelerations of a golden eagle (Aquila chrysaetos) flying in the wild, we show that the eagle's accelerations can be explained by a linear interaction with turbulence for timescales between about 1/2 and 10 s. These timescales are comparable to those of typical eagle behaviors, corresponding to between about 1 and 25 wingbeats, and to those of turbulent gusts both larger than the eagle's wingspan and smaller than large-scale atmospheric phenomena such as convection cells. The eagle's accelerations exhibit power spectra and intermittent activity characteristic of turbulence, and increase in proportion to the turbulence intensity. Intermittency results in accelerations that are occasionally several times stronger than gravity, and much larger than the ones we experience while driving, for instance. These imprints of turbulence on the bird's movements need to be further explored to understand the energetics of birds and other volant lifeforms, to improve our own methods of flying through ceaselessly turbulent environments, and to engage airborne wildlife as distributed probes of the changing conditions in the atmosphere.