In an earlier post, we talked briefly about below-ground ice and the consequences of its disappearing. However, to estimate the consequences of disappearing ground ice, one has to know that there actually is ice in the area of study. How much ice is there – and where is it? As the name suggests, below-ground ice is not so easy to spot with the naked eye. Using geophysical methods, however, ...[Read More]
Image of the Week – ROVing in the deep…
Robotics has revolutionised ocean observation, allowing for regular high resolution measurements even in remote locations or harsh conditions. But the ice-covered regions remain undersampled, especially the ice-ocean interface, as it is still too risky and complex to pilot instruments in this area. This is why it is exactly the area of interest of the paper from which our Image of the week is take ...[Read More]
Image of the Week – Bioalbedo: algae darken the Greenland Ice Sheet
Fig 1: This aerial image shows the surprisingly dark grey-brown colour of the Greenland Ice Sheet surface, around the ‘Black and Bloom’ camp. [Credit: 'Black and Bloom']
Most of the energy that drives glacier melting comes directly from sunlight, with the amount of melting critically dependent on the amount of solar energy absorbed compared to that reflected back into the atmosphere. The amount of solar energy that is reflected by a surface without being absorbed is called the albedo. A low albedo surface absorbs more of the energy that hits it compared to a high ...[Read More]
Image of the week – Learning from our past!
Figure 1: Peak global mean temperature, atmospheric CO2, maximum global mean sea level (GMSL) and source(s) of meltwater over the past 3 million years. The light blue area on each bar indicates the uncertainty associated with the maximum global mean sea level , and the pie charts denote the fraction (not location) of ice retreat in Greenland and Antarctica [Credit: Dutton et al. (2015)].
Understanding the climate evolution of our planet is not an easy task, but it is essential to understand the past if we are to predict the future! Historic climate cycles provide us with a glimpse into a period of time when the Earth was warmer than it was today. Our image of the week looks at these warmer periods of time to see what they can tell us about the future! For example, during the Plioc ...[Read More]
Image of the week – Getting glaciers noticed!
Public engagement and outreach in science is a big deal right now. In cryospheric science the need to inform the public about our research is vital to enable more people to understand how climate change is affecting water resources and sea level rise globally. There is also no better way to enthuse people about science than to involve them in it. However, bringing the cryosphere to the public is a ...[Read More]
Image of the Week – See sea ice from 1901!
Aerial photograph of the German explorer Erich von Drygalski’s ship, making its way through Antarctic sea ice. This picture was obtained from a hot air balloon in 1901. The log books of this ship were used to study sea-ice conditions at the turn of the century in the Antarctic. [Credit: National Oceanic and Atmospheric Administration/Department of Commerce]
The EGU Cryosphere blog has reported on several studies of Antarctic sea ice (for example, here and here) made from high-tech satellites, but these records only extend back to the 1970s, when the satellite records began. Is it possible to work out what sea ice conditions were like before this time? The short answer is YES…or this would be a very boring blog post! Read on to find out how hero ...[Read More]
Image of the week – Micro-organisms on Ice!
Figure 1: Investigating micro-organisms on Perito Moreno. Left – Sampling on the glacier surface inside a cryoconite hole.
Right – Scientists from the University Bicocca of Milan at work performing analysis in the temporary laboratory set up in Buscaini Refugee (shelter) [Credit: Alessio Romeo – La Venta Esplorazioni Geografiche]
The cold icy surface of a glacier doesn’t seem like an environment where life should exist, but if you look closely you may be surprised! Glaciers are not only locations studied by glaciologists and physical scientists, but are also of great interest to microbiologists and ecologists. In fact, understanding the interaction between ice and microbiology is essential to fully understand the gla ...[Read More]
Image of the Week – A new way to compute ice dynamic changes
Up to now, ice sheet mass changes due to ice dynamics have been computed from satellite observations that suffer from sparse coverage in time and space. A new method allows us to compute these changes on much wider temporal and spatial scales. But how does this method work? Let us discover the different steps by having a look at Enderby Land in East Antarctica, for which ice velocities are shown i ...[Read More]
Image of the Week – Drilling into a Himalayan glacier
Fig.1: Drilling a borehole on Khumbu Glacier, Nepal Himalaya. In the foreground, the drill stem can be seen hanging off a tripod, attached to a spool of hose. Hot, pressurised water is supplied to these units from a pressure-washer in the background. [Credit: Katie Miles]
How water travels through and beneath the interior of debris-covered glaciers is poorly understood, partly because it can be difficult to access these glaciers at all, never mind explore their interiors. In this Image of the Week, find out how these aspects can be investigated by drilling holes all the way through the ice… Hydrological features of debris-covered glaciers Debris-covered glaciers ca ...[Read More]
Image of the Week – Fifty shades of snow
Fig. 1: Green snow [Credit: NASA's Earth Observatory]
When I think of snow, I tend to either think about the bright white ski slopes in the mountains or the large white areas in the Arctic. However, natural phenomena can lead to colorful snow. Our Image of the Week shows snow can be green! Snow can also turn orange, pinkish, grey and even yellow… But where do these different shades of snow come from? White The most common color of snow is white (see ...[Read More]