Photo Friday: Shiveluch Volcano Eruption in Siberia

Shiveluch Volcano, a super volcano in Siberia, erupted on Wednesday. The volcano is located in the northernmost portion of the glacier-covered volcano belt in the Russian Far East called the Kamchatka Krai. Although no locals were believed to be impacted by the blast, the Shiveluch eruption spewed ash 10 kilometers into the sky. The ash cloud has reportedly been extended to a length of 100 kilometers, chiefly in the southeastern direction. An “Orange” aviation warning was issued by the Kamchatka Volcanic Response Team. Airlines were advised to change their flight routes as ash particles could stall the aircraft’s engine. The Russian volcano service had also issued volcanic ash advisories since early November. Prior to this event, Shiveluch erupted almost a decade ago in March 2007.

 

Lava fresh out of the vent (Source: BirGün Gazetesi/Twitter)
Lava fresh out of the vent (Source: BirGün Gazetesi/Twitter).

 

Ash spewing from the glacier covered Shiveluch Volcano (Source: İhlas Son Dakika / Twitter)
Ash spewing from the glacier covered Klyuchevskoy Volcano (Source: İhlas Son Dakika/Twitter).

 

Satellite view of the ash cloud (Source: NASA).

 

The pristine view of the Shiveluch Volcano before its eruption (Source: Uykoal/Instagram)
The pristine view of the Klyuchevskoy Volcano before its eruption (Source: Uykoal/Instagram).
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Roundup: Siberia, Serpentine and Seasonal Cycling

Roundup: Siberian Glaciers, Vegetation Succession and Sea Ice

 

Glaciers in Siberia During the Last Glacial Maximum

From Palaeogeography, Palaeoclimatology, Palaeoecology: “It is generally assumed that during the global Last Glacial Maximum (gLGM, 18–24 ka BP) dry climatic conditions in NE Russia inhibited the growth of large ice caps and restricted glaciers to mountain ranges. However, recent evidence has been found to suggest that glacial summers in NE Russia were as warm as at present while glaciers were more extensive than today… We hypothesize that precipitation must have been relatively high in order to compensate for the high summer temperatures… Using a degree-day-modelling (DDM) approach, [we] find that precipitation during the gLGM was likely comparable to, or even exceeded, the modern average… Results imply that summer temperature, rather than aridity, limited glacier extent in the southern Pacific Sector of NE Russia during the gLGM.”

Read more about the study here.

 

Siberia experiences very cold temperatures but has relatively few glaciers (Source: Creative Commons)
Siberia experiences very cold temperatures but has relatively few glaciers (Source: Creative Commons).

 

Plant Communities in the Italian Alps

From Plant and Soil: “Initial stages of pedogenesis (soil formation) are particularly slow on serpentinite… Thus, a particularly slow plant primary succession should be observed on serpentinitic proglacial (in front of glaciers) areas..Ssoil-vegetation relationships in such environments should give important information on the development of the “serpentine syndrome” .Pure serpentinite supported strikingly different plant communities in comparison with the sites where the serpentinitic till was enriched by small quantities of sialic (rich in silica and aluminum) rocks. While on the former materials almost no change in plant species composition was observed in 190 years, four different species associations were developed with time on the other. Plant cover and biodiversity were much lower on pure serpentinite as well.”

Read more about “serpentine syndrome” here.

 

Plant communities in the Italian Alps can differ depending on the underlying bed rock (Source: Creative Commons)
Plant communities in the Italian Alps can differ depending on the underlying bed rock (Source: Creative Commons).

 

Carbon Cycling and Sea Ice in Ryder Bay

From Deep Sea Research Part II: Topical Studies in Oceanography: “The carbon cycle in seasonally sea-ice covered waters remains poorly understood due to both a lack of observational data and the complexity of the system… We observe a strong, asymmetric seasonal cycle in the carbonate system, driven by physical processes and primary production. In summer, melting glacial ice and sea ice and a reduction in mixing with deeper water reduce the concentration of dissolved organic carbon (DIC) in surface waters… In winter, mixing with deeper, carbon-rich water and net heterotrophy increase surface DIC concentrations… The variability observed in this study demonstrates that changes in mixing and sea-ice cover significantly affect carbon cycling in this dynamic environment.”

Read more about carbon cycling in West Antarctica here.

 

Seasonal sea ice melting influences the cycling of carbon in West Antarctica (Source: Jason Auch / Creative Commons).
Seasonal sea ice melting influences the cycling of carbon in West Antarctica (Source: Jason Auch/Creative Commons).
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Roundup: Climate Science and International Adaptation

Integration of Glacier and Snow

“Energy budget-based distributed modeling of snow and glacier melt runoff is essential in a hydrologic model to accurately describe hydrologic processes in cold regions and high-altitude catchments. We developed herein an integrated modeling system with an energy budget-based multilayer scheme for clean glaciers, a single-layer scheme for debris-covered glaciers, and multilayer scheme for seasonal snow over glacier, soil, and forest within a distributed biosphere hydrological modeling framework.”

Read more of the article here.

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Climate Science on Glaciers

“The 2001–2013 sum of positive temperatures (SPT) record, as a proxy of snow/ice ablation, has been obtained for the high-mountain glaciarized Munku-Sardyk massif, East Sayan Mountains, using daily NCEP/NCAR reanalysis data. The SPT (and ice melt) demonstrates a significant decreasing trend, with the highest values in 2001, 2002, and 2007, and the lowest in 2013. We have investigated relationships between potential summer ablation and synoptic-scale conditions over the study area.”

Read more of this article here.

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International Adaptation to Glacier Retreat

“The transboundary Himalayan Rivers flowing through Bhutan to India and Bangladesh constitute an enormous asset for economic development in a region which contains the largest number of poor people in the world. However, the rapid retreat of Himalayan glaciers has made South Asia vulnerable to variety of water-related natural hazards and disasters such as floods, landslides, and glacial lake outburst.”

Read more of this book chapter here.

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