Time & Space of Glaciers

Glaciers-Time-and-Space-Blog-Cover-Image Ice fall in Azay glacier. Photo credit Alexandra Rogozhina & IGRAS/RGO.

People usually perceive space and time by comparing them to their own life. Words such as “forever” and “until the end” appear in fiction. But how can we imagine the space and time of the mountain glaciers whose existence goes beyond our usual perception? And why is it so important for us now? In this blog post, researcher Alexandra Rogozhina shares her thoughts on these suggestive topics.

Mostly, when we hear about the loss of glaciers, it is regarding climate change. Undoubtedly, glaciers are the most sensitive indicators of climate change. They make these changes visible to us. Most often information about ice loss is presented in the form of graphics and diagrams. Or sometimes only with calculations and numbers. But we can’t imagine the real picture of the process and the scale of the reduction of the glaciers. Thus, it’s also impossible to link these changes to things we are familiar with and present it to people outside of science or mathematics.

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Garabashi glacier, Elbrus mountain, 2013 & 2020. Photo credits: Alexandra Rogozhina.

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Djhankhyat glacier, Elbrus mountain region, 1967 & 2000. Photo credits: Alexandra Rogozhina & IGRAS/RGO.

For a few years I have been looking at the glaciers in the Caucasus Mountain Region as a mountaineer and snowboarder. When I saw the glaciers of Elbrus Mountain every day, I started noticing visible changes. When I spoke with the locals about those changes, they showed me where the glacier was during different stages of their life. I was very keen to find the ancient images of the glaciers and make those changes clear for everyone. The magnificence and fragility of the glaciers has always inspired me to look deeper into them.

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Rocks in a place of Azay glacier ice fall in 1932 & 2020. Photo credits: Alexandra Rogozhina & IGRAS/RGO.

Repeat photography

Usually, in science articles we can see two photos of the same glacier in the late 19th century and today. We can see the difference of 100 years as a result of climate change. But I wanted to show the process, and how this change happened over time. It was very difficult and tedious work to find the images of the same glacier from the same angles. It doesn’t have to be a photo image. It might also be a life drawing, engraving, lithography, daguerreotype image, postcard, stereo photo pair, card, newspaper article and any other type of image. The main idea is that presenting these images in a row for a certain glacier can provide us with the information about its past and tell us its real life story.

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Shelda glacier, Elbrus mountain region, 1886 & 1934. Credits: Alexandra Rogozhina & IGRAS/RGO.

Today, scientists are aware of the state of the mountain glaciers at the beginning of the Holocene (approximately 11,600 years ago) and during the Little Ice Age (1700-1900). By using the spatio-temporal reconstructions from scientists with historical images of the glaciers, we can visualize their history in the past 150-200 years. We can see how great they were at the end of the Little Ice Age and the evolutionary path of their changes until today. In the period of the Anthropocene, and such extreme climate changes, it is very important to understand how glaciers lose mass. Moreover, the visual reconstruction of the glaciers provides us with information prior to direct instrumental observations. Whilst one human’s lifetime only spans a little part of a glacier’s life, many generations of humans can see the changes. Glaciers appeared on the Earth before humans, and some will be here after us, but in what shape or size?

Lifelines

Sometimes I get sad when I look at the glaciers’ lifelines carved into the rock like the lifelines on a palm of a human. Trimlines are the typical marks left by the glaciers on the borders of the valley. These lines show us where the glacier was located in the past, but it is still hard to understand what happened with them 150 years ago, because the time and space of a human life is very different to that of a living glacier. This difference is shown by rows of historical images of mountain glaciers.

Now I am beginning to collect the Alpine glacier images and I’m open for offers and collaborations, if you are interested, please reach out!


This blog post was written by Alexandra Rozoghina and edited by Jenny Turton, Hayat Nasirova, and Giovanni Baccolo. It was first published on the EGU Blogs website, and is reproduced here under the Creative Commons Attribution 4.0 International licence (CC BY 4.0).

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