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Pacific Walruses Studied as Sea Ice Melts


Pacific Walruses Studied as Sea Ice Melts

ANCHORAGE, Alaska — USGS Alaska Science Center researchers, in cooperation with the Native Village of Point Lay, will attempt to attach 35 satellite radio-tags to walruses on the northwestern Alaska coast in August as part of their ongoing study of how the Pacific walrus are responding to reduced sea ice conditions in late summer and fall.

Walruses spend most of their lives at sea, but haul out on sea ice and sometimes land to rest between feeding bouts.  They can dive hundreds of feet to forage on the sea floor. However, when the sea ice recedes past the continental shelf into very deep waters of the Arctic Basin, the walruses haul out on land.  The extent of sea ice has been less in recent summers, and walruses have been hauling out on beaches in Alaska and Russia in the past few years. Thus, radio-tracking the walruses’ movements in water and to and from land provides important insights into walrus movements and foraging behaviors in response to changing sea ice conditions.

Since 2004, the USGS Alaska Science Center Pacific Walrus Research Program has collected data on walrus foraging behavior and movements throughout areas of the Bering and Chukchi seas during periods when sea ice is present and when sea ice is absent over the continental shelf.  In 2010, walruses came ashore in late August. This year, the sea ice disappeared from the shelf earlier and walruses have already begun to come ashore.

“Sea ice is an important component in the life cycle of walruses,” said Chad Jay, research ecologist with the USGS Alaska Science Center. “These tracking studies will help us to better understand how top consumers in the arctic ecosystem may be affected by changes in sea ice habitats.”

In July, the scientists attached 40 radio tags on walruses hauled out on distant offshore sea ice near the edge of the continental shelf, northwest of Barrow, Alaska. This month researchers will tag a number of walruses that have come to land after the retreat of the sea ice from the shelf. Tracking animations from tagged walruses are available online and are updated approximately every week.

For photos and more information related to the USGS Pacific walrus studies visit http://www.usgs.gov/blogs/features/

USGS Newsroom


More information

Parameter Value Description
Magnitude mb The magnitude for the event.
Longitude ° East Decimal degrees longitude. Negative values for western longitudes.
Latitude ° North Decimal degrees latitude. Negative values for southern latitudes.
Depth km Depth of the event in kilometers.
Place Textual description of named geographic region near to the event. This may be a city name, or a Flinn-Engdahl Region name.
Time 1970-01-01 00:00:00 Time when the event occurred. UTC/GMT
Updated 1970-01-01 00:00:00 Time when the event was most recently updated. UTC/GMT
Timezone offset Timezone offset from UTC in minutes at the event epicenter.
Felt The total number of felt reports
CDI The maximum reported intensity for the event.
MMI The maximum estimated instrumental intensity for the event.
Alert Level The alert level from the PAGER earthquake impact scale. Green, Yellow, Orange or Red.
Review Status Indicates whether the event has been reviewed by a human.
Tsunami This flag is set to "1" for large events in oceanic regions and "0" otherwise. The existence or value of this flag does not indicate if a tsunami actually did or will exist.
SIG A number describing how significant the event is. Larger numbers indicate a more significant event.
Network The ID of a data contributor. Identifies the network considered to be the preferred source of information for this event.
Sources A comma-separated list of network contributors.
Number of Stations Used The total number of Number of seismic stations which reported P- and S-arrival times for this earthquake.
Horizontal Distance Horizontal distance from the epicenter to the nearest station (in degrees).
Root Mean Square sec The root-mean-square (RMS) travel time residual, in sec, using all weights.
Azimuthal Gap The largest azimuthal gap between azimuthally adjacent stations (in degrees).
Magnitude Type The method or algorithm used to calculate the preferred magnitude for the event.
Event Type Type of seismic event.
Event ID Id of event.
Event Code An identifying code assigned by, and unique from, the corresponding source for the event.
Event IDS A comma-separated list of event ids that are associated to an event.

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