WERC

Mat Wooller (Alaska Stable Isotope Facilty), Jim Shobe (PhD graduate student) and Terry Smith (North Pole high school student intern) (l to r) test a new vibra-coring system through a hole in lake ice to sample long cores of sediment beneath a thaw lake near the UAF campus.

UAF photo by Todd Paris.

Sveta Berezoskaya and Romain Provost measure stream flow of a small creek near Barrow.

Credit: Anna Liljedahll

Drunken trees in a black spruce forest near Fairbanks, Alaska. As permafrost thaws, the ground subsides, and surface moisture conditions can become too wet for the trees to survive.

Credit: Miriam Jones

Thermokarst lakes in the Yukon-Kuskokwim Delta.

Credit: Miriam Jones

The rhizones pictured above are used to extract microbe samples from the sediment core. The microbes being studied are responible for producing and oxidizing methane.

Credit: Mat Wooler

The wind near Barrow, Alaska has carved and packed this snow surface.

Credit: Sveta Berezovskaya

Douglasia ochotensis grows 30 miles south of Prudehoe Bay, Alaska. It is one of the first flowers to bloom in the Arctic sometime in June.

Credit: Sveta Berezovskaya

Joel Bailey and Peter Prokein install equipment that will send weather data back to the University of Alaska Fairbanks some 200 miles to the south.

Credit: Sveta Berezovskaya

Rainbow over a peatland in the Susitna Valley, just to the south of the Alaska Range.

Credit: Miriam Jones

The Alyeska oil pipeline seen from an altitude of 500 feet about 20 miles south of Prudhoe Bay. The pipeline acts as a snow fence which retains more snow than the surrounding tundra.

Credit: Sveta Berezovskaya

The polygonal fractures in this tundra near the Deadhorse airport are caused by repeated thawing and freezing.

Credit: Sveta Berezovskaya

Robert Gieck and Joel Homan take stream flow measurements with a hand held FlowTracker in late May 2007

Credit: Sveta Berezovskaya

Weather conditions in early April cultivate this rime ice on a precipitation gauge in Barrow. Rime forms when supercooled droplets collect and rapidly crystalize on a surface.

Credit: Sveta Berezovskaya

Thermally-grown ice becoming 'candled' as it decays on an Arctic lake south of Deadhorse on June 9, 2009.

Credit: Sveta Berezovskaya

Itkillik River surface water monitoring station, view from the bluff, near the northern foothills of the Brooks range

Credit: Emily Youcha

Massive ice wedge on near Cape Espenberg.

Credit: Miriam Jones

Permafrost degradation on the southern Seward Peninsula. The lake formed as a previously frozen ice wedge thawed.

Credit: Miriam Jones

Rainbow on the southern Seward Peninsula.

Credit: Miriam Jones

25

Sep

Imiq: a hydroclimate database and data portal for Alaska

WERC will host its first seminar of the semester this Friday, September 26, 2014 at 3:30pm in Duckering 531. Jessie Cherry and Amy Jacobs will kick off the season presenting their efforts on creating a hydroclimate database and data portal for Alaska. (more…)

18

Sep

Chas Jones PhD defense: Connecting the dots between hydrology, climate, and people of the North

Chas Jones will be defending his Ph.D. dissertation titled “Ecohydrological Linkages: Connecting the dots between hydrology, climate, and people of the North” on Monday, Sept. 29 at 2:30pm at the Murie Auditorium. (more…)

8

Oct

WERC Request for Research Articles

Announcing an opportunity for any student who is associated with a WERC- related research project to submit articles detailing current research and receive $50 as compensation. (more…)