The Meteorology on the Debris-Covered Tongue of Kennicott Glacier, Wrangell Mountains -- from the Micro to the Macro Sca

Debris-covered glaciers are characterized by a continuous layer of rock material on their tongue and surface. Pascal Buri, Martin Truffer, Javier Fochesatto, and Andy Aschwanden, UAF

Debris-covered glaciers are characterized by a continuous layer of rock material on their tongue and surface energy balance models are commonly used to estimate melt rates of these glaciers. This requires direct on-glacier measurements of energy fluxes that are rare in many mountain ranges globally and completely absent in Alaska.

Using observations from weather stations installed in the middle of the Kennicott Glacier tongue (Wrangell Mts.) during the 2019 melting season, we assess for the first time the meteorological conditions on a debris-covered glacier tongue in Alaska. We measured temperature, humidity and wind speeds at different levels above the debris, as well as turbulent fluxes, solar and long-wave emitted radiation and precipitation. For comparison to off-glacier meteorological conditions we use data from a nearby station installed outside the glacier impacted by the same meteorological fields.

We observed a strong heating rate in the debris-covered surface during the day, while radiative cooling occurred overnight. This nocturnal effect prevents the underlying ice from the accelerated daytime melting enhanced by the debris. Additionally, we found that the heat exchange over debris strongly contrasted the conditions over the debris-free surface on-glacier, as well as the terrain surrounding the valley glacier. The experimental determination of turbulent fluxes (sensible and latent heat) play an important role in precising the energy budget of debris glaciers. However, these observations are difficult because the turbulence regime over the glacier tongue is affected during the melting season due to the appearance and backwasting of crevasses and ice faces. Pascal Buri, Martin Truffer, Javier Fochesatto, and Andy Aschwanden, UAF

Part of a series of articles titled
Copper River Basin Symposium - Wrangell-St Elias National Park and Preserve.

Previous:
Continuous Climate Data Collection in Wrangell-St. Elias National Park and Preserve: Lessons Learned and Emerging Trends.

Next:
Preliminary Results from the Excavation of NAB-533, a Multi-Component Prehistoric Archaeological Site in the Northern Copper River Basin.

Where this belongs

• Wrangell - St Elias National Park & Preserve

Where this page came from

This page was imported from National Park Service. Produced by the U.S. National Park Service and, as a work of the United States government, in the public domain.

Nobody has written it yet — it is the source material at a new address, which is why search engines are asked to skip it and why no one earns from it. It is up for grabs: take it on, and it is yours to rewrite and to earn from.