Polar bears live in high-latitude environments characterized by cyclic vari
ation in form and extent of sea ice. From 1991 to 1995, we used radio telem
etry and monthly satellite images to compare patterns of ice selection by 1
10 female polar bears, relative to two geographic regions and four seasons.
We hypothesized that extreme seasonal changes in ice characteristics in th
e Baffin Bay region, including a period of open water, may limit polar bear
density despite supporting greater prey density than the Archipelago regio
n, where ice is present year-round. Using cyclic time series analysis to mo
del seasonal variation, we found differences in level, amplitude, and phase
between sea ice characteristics and habitat selection by polar bears of th
e Arctic Archipelago and Baffin Bay regions. Polar bears not only followed
seasonal changes, but they anticipated seasonal fluctuations, e.g., polar b
ears were found close to ice edges in spring in advance of the peak availab
ility of edges. Also, seasonal selection of sea ice by polar bears was gene
rally of a larger amplitude than cycles in ice and is best explained by int
ensive use of specific ice types in spring and summer, and sparse use durin
g the remaining year. During spring and summer, Archipelago bears used land
fast ice more intensively, whereas Baffin bears used moving ice, defined as
thick first-year ice found in large flees. Both ice types likely represent
areas where most seal pupping occurred in spring for each region. Bears fr
om both regions selected first-year ice in winter when new ice was forming
and multiyear ice in autumn when maximum ice melt had occurred. Overall, po
lar bear selection of ice habitat was similar between regions despite major
differences in seasonal ice characteristics. Polar bear density may not di
rectly relate to prey density, due to the limited ability of bears to track
the extreme seasonal fluctuations in ice extent found in more productive e
nvironments.