Imaggeo on Mondays: Mount Yasur

November 14, 2011

Strombolian activity on Mount Yasur, Vanuatu. Image by Derya Gürer, distributed by EGU under a Creative Commons licence.

Imaggeo is the online open access geosciences image repository of the European Geosciences Union. Every geoscientist who is an amateur photographer (but also other people) can submit their images to this repository. Being open access, it can be used by scientists for their presentations or publications as well as by the press. If you submit your images to imaggeo, you retain full rights of use, since they are licenced and distributed by EGU under a Creative Commons licence.


EGU General Assembly 2012 Call for Papers

November 9, 2011

Abstract submission for the EGU General Assembly 2012 (EGU2012) is now open. The General Assembly is being held from Sunday 22 Apr 2012 to Friday 27 Apr 2012 at the Austria Center Vienna, Austria.

You can browse through the Sessions online.

Each Session shows the link Abstract Submission. Using this link you are asked to log in to the Copernicus Office Meeting Organizer. You may submit the text of your contribution as plain text, LaTeX, or MS Word content. Please pay attention to the First Author Rule.

The deadline for the receipt of Abstracts is 17 January 2012. In case you would like to apply for support, please submit no later than 15 December 2011. Information about the financial support available can be found on the Support and Distinction part of the EGU GA 2012 website.

Further information about the EGU General Assembly 2012 on it’s webpages. If you have any questions email the meeting organisers Copernicus.


Imaggeo on Mondays: Lava flow into sea

November 7, 2011

Lava from the East Rift Zone entering the sea near Kalapana (Hawaii Big Island). Image by Martin Mergili, distributed by EGU under a Creative Commons License.

The image shows a flow of basaltic lava out of a lava tunnel into the sea. The location of the scene is the shoreline of Hawaii Big Island near the village of Kalapana. Flow direction of the lava is from the bottom to the top of the image, vaporization of sea water leads to a steam plume of considerable size. Originating from the East Rift Zone, many of the lava flows in that area occur beneath a layer of partially solidified lava. The image was taken on August 13, 2010 during a touristic helicopter flight on a holiday trip.

Imaggeo is the online open access geosciences image repository of the European Geosciences Union. Every geoscientist who is an amateur photographer (but also other people) can submit their images to this repository. Being open access, it can be used by scientists for their presentations or publications as well as by the press. If you submit your images to imaggeo, you retain full rights of use, since they are licenced and distributed by EGU under a Creative Commons licence.


Geosciences column: Iceland spar, or how Vikings used sunstones to navigate

November 2, 2011

by Bárbara Ferreira, EGU’s Media and Communications Officer

Nowadays, we can rely on GPS receivers or magnetic compasses to tell us how to reach our destination. Some 1000 years ago, Vikings had none of these advanced navigation tools. Yet, they successfully sailed from Scandinavia to America in near-polar regions where it can be hard to use the Sun and the stars as a compass. Clouds or fog and the long twilights characteristic of polar summers complicate direct observations of these celestial bodies. So how did they find their bearings? A new study published in Proceeding of Royal Society A shows that they probably used Iceland spar, a “sunstone”.

Centuries-old Viking legends tell of glowing sunstones that navigators used to find the position of the Sun and set the ship’s course even on cloudy days. In 1967, a Danish archaeologist named Thorkild Ramskou speculated that the Viking sunstone could have been Iceland spar, a clear variety of calcite common in Iceland and parts of Scandinavia.

This crystal has an interesting property called birefringence: a light ray falling on calcite will be divided in two, forming a double image on its far side. (This double image is easily seen by placing transparent calcite on printed text.) Further, the Iceland spar is a polarising crystal, meaning the two images will have different brightnesses depending on the polarisation of light.

Birefringence of Iceland Spar seen by placing it upon a paper with written text. Source: Wikimedia Commons.

Light is made up of electromagnetic waves with component electric and magnetic fields. If these components have a specific orientation, the light is said to be polarised, while in unpolarised light the orientation of these fields has no preferred direction. Calcite can appear dark or light depending on the polarisation of light that falls upon it.

Sunlight becomes polarised as it crosses the Earth’s atmosphere, and the sky forms a pattern of rings of polarised light centred on the Sun. Changing the orientation of calcite as light passes through it will change the relative brightness of the projections of the split beams, even when the Sun is hiding behind clouds or just below the horizon. The beams are equally bright when the crystal is aligned to the Sun.

It can be hard to determine when exactly these split beams have equal brightness. But the new study, led by Guy Ropars at the University of Rennes 1 in France, suggests Vikings could have built a simple device to better use the sunstone.

The technique consists in covering the Iceland spar with an opaque screen with a small hole in its centre and a pointer. As light passes through the hole onto the crystal, a dark surface below it receives the projection of the double image for comparison.

The authors of the Proceedings of the Royal Society study believe Vikings could have used a device like this to navigate. The crystal is inside, and the projection of a double image is seen below it. Credit: Guy Ropars. Source: ScienceNOW.

By rotating the apparatus and determining the direction at which the two images were equal in brightness, the team managed to pinpoint the Sun’s position on a cloudy day with an accuracy of one degree on either side. Researchers also conducted tests when the Sun was largely below the horizon. “We have verified that the human eye can reliably guess clearly the Sun direction in dark twilights, even until the stars become observable,” Ropars’ team writes in the paper.

Although archaeologists have not yet found Iceland spar among Viking shipwrecks, the new study adds credence to the idea that Viking seafarers used the crystal in their travels.

Further, the recent finding of a calcite crystal on a sixteenth century Elizabethan ship shows that navigators could have used Iceland spar even after the appearance of the magnetic compass. Cannons on ships could perturb a magnetic compass orientation by 90 degrees, so a crystal serving as an optical compass could be crucial in avoiding navigational errors and get sailors to a safe port.


Imaggeo on Mondays: Napoli and Vesuvio

July 18, 2011

The volcano Vesuvio, Napoli in the foreground, view from Castel Sant’Elmo. Image by Martin Mergili, distributed by EGU under a Creative Commons License.

Imaggeo is the online open access geosciences image repository of the European Geosciences Union. Every geoscientist who is an amateur photographer (but also other people) can submit their images to this repository. Being open access, it can be used by scientists for their presentations or publications as well as by the press. If you submit your images to imaggeo, you retain full rights of use, since they are licenced and distributed by EGU under a Creative Commons licence.


Call for Sessions for EGU General Assembly 2012

July 8, 2011

The public call for sessions for the European Geosciences Union General Assembly 2012 has been issued. The EGU GA 2012 will be held at the Austria Center Vienna (ACV) from 22 April to 27 April 2012. The details are below, the web page to visit to submit sessions is Call for Sessions page of the EGU General Assembly 2012 website.

We hereby invite you, from now until 16 Sep 2011, to take an active part in organizing the scientific programme of the conference.

Please suggest (i) new sessions with conveners and description and (ii) modifications to the skeleton programme sessions. Explore the Programme Groups (PGs) on the left hand side, when making suggestions. Study those sessions that already exist and put your proposal into the PG that is most closely aligned with the proposed session’s subject area.

If the subject area of your proposal is strongly aligned with two or more PGs, co-organization is possible and encouraged between PGs. Only put your session proposal into one PG, and you will be able to indicate PGs that you believe should be approached for co-organization.

If you have questions about the appropriateness of a specific session topic, please contact the Officers for the specific EGU2012 Programme Group. To suggest Union Symposia, Great Debates, Townhall Meetings or Short Courses, please contact the Programme Committee Chair (Gert-Jan Reichart).

In case any questions arise, please contact EGU2012 at Copernicus.


Imaggeo on Mondays: Damavand Volcano

July 4, 2011

Damavand Volcano, Iran. A nice cap cloud can be seen at the top of the mountain. Cap cloud is an orographic cloud that is formed over a mountain peak, formed by the cooling and condensation of moist air climbing up and over the peak. Cap clouds appear to remain stationary. Image by Mostafa Ganjian, distributed by EGU under a Creative Commons License. Commentary by Konstantinos Kourtidis.

Imaggeo is the online open access geosciences image repository of the European Geosciences Union. Every geoscientist who is an amateur photographer (but also other people) can submit their images to this repository. Being open access, it can be used by scientists for their presentations or publications as well as by the press. If you submit your images to imaggeo, you retain full rights of use, since they are licenced and distributed by EGU under a Creative Commons licence.


Grímsvötn eruption and the importance of research

May 26, 2011

This perspective on the Grímsvötn eruption and volcanic activity, ash transport and ash detection comes from Dr Mike Burton. Dr Burton is a Senior Researcher at the Istituto Nazionale di Geofisica e Vulcanologia, Pisa, Italy. His research includes utilising novel gas and video imaging techniques to better understand volcanic processes. At the EGU General Assembly 2011, he convened GMPV5 Monitoring and observations of active volcanoes using in-situ and remote sensing techniques along with Thomas Staudacher , Jurgen Neuberg , Hugo Delgado Granados, and Alessandro Bonaccorso.”

Once more with feeling
Just a little more than a year after the eruption of Eyjafalla another Icelandic volcano, Grímsvötn, is injecting volcanic ash and gas high into the atmosphere, disrupting air traffic over Europe. This time the eruption has been much more intense, with an eruption column reaching up to 20 km in the initial stages of the activity. Fortunately the eruption has swiftly waned, and at the time of writing eruptive activity has reduced greatly. Nevertheless, the volcanic ash already injected into the upper troposphere will continue to circulate for several days before it becomes so dilute that it no longer poses a risk to aviation, and we see that airports in northern Europe have had to close as air traffic restrictions are put in place. Such events remind us of the enormous importance that European level research in volcanic activity, ash transport and ash detection has for improving our ability to both understand and react to rapidly changing events.

Volcanic eruptions, while challenging to predict, are produced from well-known areas, particularly in Iceland where frequent eruptions have been extremely well-documented and well-observed for many years. This allows statistical analysis of the frequency of such events and preparation for their eventuality. Unfortunately, while scientists from many nations have lobbied for increased resources to deal with this issue, governments have been slow to act, but the recent eruptions on Iceland and their consequent impact on the European economy through disruption to air traffic has produced an unprecedented focus on this issue. This focus was exemplified at the recent EGU General Assembly in Vienna in April where a series of well-attended sessions focussed on the science of the 2010 eruption, modelling of the ash dispersal and analysis of satellite and lidar measurements of ash. It is clear that further research is a fundamental priority for Europe in order to produce improving responses to the inevitable eruptions which will occur in the future, not just from Iceland, but also from Italy and potentially the Azores and Canary Islands as well.


Grimsvötn eruption observations from the field

May 26, 2011

This description on the Grímsvötn eruption comes from Dr Olgeir Sigmarsson, an Icelandic volcanologist who is Director of Research, CNRS at the Laboratoire Magmas et Volcans, Observatoire de Physique du Globe de Clermont-Ferrand. He also works at the Institute
of Earth Sciences, University of Iceland. His research is on geochemistry: genesis, chronology and evolution of magma. Dr Sigmarsson has been collecting tephra samples from the glacier in the field near to the Grimsvötn volcano and the below contains information from his Icelandic colleagues.

The Grimsvötn eruption 2011 has stopped for the time being. It started around 19:00 last Saturday (21 May) and it’s eruption column rose to approximately 17 km during the first night. It thus penetrated into the stratosphere, observed for the first time for an eruption from Grimsvötn volcano. Grimsvötn is a complex caldera structure covered by the largest ice-cap in Europe, namely Vatnajökull. The high-temperature area melts the floating ice on the subglacial lake that occasionally is lifted from the bedrock by the water mass, emptying the lake and creating glacier bursts, better known as jökulhlaup. Such pressure release generates more vigorous boiling in the geothermal system and sometimes may act as a trigger for an eruption (such as in the 2004 eruption). Fortunately the last jökulhlaup occurred last autumn, leaving little water in the subglacial caldera lake.

The actual eruption emitted approximately 10-20 tons/sec of tephra during the first day but declined rapidly and on the 24th May the column rose only to 3 km height during occasional explosions. On the 4th day, only vapour explosions with little solid material were observed at the crater close to the south wall of the caldera. Tephra fall was noticed all over Iceland (with the exception of the Westfjord peninsula) with grain-size having approximately 10% finer than 10 micronmeters and 50% finer than 50 micronmeters. Based on preliminary measured tephra thickness, the volume is crudely estimated as ½ cubic km of freshly fallen tephra.

Seismicity and deformation indicate a shallow magma source and the magma is basaltic of quartz-normatve tholeiite composition similar to all historic tephra. However, since the Laki eruption, increased concentrations of incompatible elements have increased with time suggesting a closed-system behaviour with minimal deeper input of more primitive magma. The fact the actual eruption was very explosive in the beginning and rose above the tropopause indicate either (1) a more evolved basaltic magma than before or (2) a deeper gas-rich magma entering into the plumbing system beneath Grimsvötn caldera. The first possibility would suggest that the volcano is evolving towards more evolved magma with higher gas content
and potential high explosivity, whereas the second possibility suggests a changing feeding system with renewal of fresh basalt from depth. These two possibilities can be distinguished by precise trace element analysis of the actual tephra.


Grímsvötn volcanic eruption

May 24, 2011

The Grímsvötn volcano in Iceland started erupting on 21 May 2011. Icelandic airspace was closed soon after with flights now being affected in the United Kingdom.

This post brings together some good sources of imagery and information. These sources are not endorsed by the European Geosciences Union, more a resource letting people know what is available. If you know of a good source of information, let us know in the comments or email us.

The UK Met Office is responsible for ash cloud monitoring for Northern European airspace. Their pages include warnings issues and maps showing predicted ash cloud movements.

NASA Earth Observatoryimagery is available (such as below). Including commentary on the image.

Grímsvötn Modis Natural-Color Image (NASA, 2011)

The European Organisation for the Exploitation of Meteorological Satellites (EUMETSAT) has imagery and animcationsfrom various satellites, including real-time images. An example is shown below.

Grímsvötn Altitude Imagery, copyright EUMETSAT (2011)

Grímsvötn Altitude Imagery, copyright EUMETSAT (2011)

News and information from Iceland itself is available from the Iceland Met Office and the University of Iceland Institute of Earth Sciences which has an Eruption in Grímsvötn 2011 page, which contains photos, satellite imagery, GPS time series, chemical composition information, and relevant scientific publications alongside status reports.

Relevant abstracts about the Grímsvötn volcano that were presented at the EGU General Assembly 2011 are Óladóttir et al., Thordarson et al., and Magnússon et al..


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