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A first-timer’s guide to the 2017 General Assembly

A first-timer’s guide to the 2017 General Assembly

Will this be your first time at an EGU General Assembly? With 13,650 participants in a massive venue, the conference can be a confusing and, at times, overwhelming place.

To help you find your way, we have compiled an introductory handbook filled with history, presentation pointers, travel tips and a few facts about Vienna and its surroundings. Download your copy of the EGU General Assembly guide here!

Imaggeo on Mondays: Don’t miss the abstract deadline

Imaggeo on Mondays: Don’t miss the abstract deadline

The EGU General Assembly brings together geoscientists from all over the world to one meeting that covers all disciplines of the Earth, planetary and space sciences. The conference is taking place in Vienna on 23–28 April 2017, providing an opportunity for both established scientists and early career researchers to present their work and discuss their ideas with experts in all fields of the geosciences.

You can get a feel for the great geoscience that will be discussed at the meeting by browsing through the EGU 2017 sessions. Clicking on ‘please select’ allows you to search for sessions by Programme Group. You’ll then be able to view the sessions in more detail and submit an abstract to its relevant session. The deadline for abstract submission is 11 January 2017, 13:00 CET. That’s only two days away!

Also, remember that you can benefit from early registration for the conference until 31 March 2017. Register online on the Registration section of the General Assembly website. Note that EGU members benefit from reduced member rates; to become a member, or renew your EGU membership, go to www.egu.eu/membership/.

The full meeting programme will be made available on 2 March 2017.

For more information about the General Assembly, please see the EGU 2017 website.

Note on hotel reservations
Please note that the congress ECCIMD2017 (10,000 participants) will take place in Vienna at the same time as the EGU2017. In addition, the Vienna City Marathon (40,000 participants) will take place on Sunday, resulting in many hotels being fully booked the night before. Therefore, we strongly recommend booking accommodation as soon as possible.

Try something different – choose a PICO session at EGU 2017!

Try something different – choose a PICO session at EGU 2017!

Some of the sessions scheduled for the upcoming EGU General Assembly are PICO only sessions. This means that, rather than being oral or poster format, they involve Presenting Interactive COntent (PICO). The aim of these presentations is to highlight the essence of a particular research area – just enough to get the audience excited about a topic without overloading them with information.

What’s great about this format is that it combines the best of oral and poster presentations.  It allows researchers to stand up and be recognised for great research while giving an oral contribution as well as discussing their work in detail and networking with other participants.

PICO sessions start with a series of 2 minute long presentations – one from each author. They can be a Power Point, a movie, an animation, or simply a PDF showing your research on a display. After the 2 minute talks, the audience can explore each presentation on touch screens, where authors are also available to answer questions and discuss their research in more detail.

Presenting a PICO for the first time can be daunting, so we’ve prepared a guide which talks you through the format step-by-step. It’s packed with practical tips on the best layout for your PICO, how to capture the audience’s attention in just two minutes and how to get the most out of the discussion at the interactive screen.

And don’t forget, as of the 2016 General Assembly, PICO presentations are part of the Outstanding Student Poster and PICO (OSPP) Awards. To be considered for the OSPP award, you must be the first author and personally present the PICO at the conference:

  • being a current undergraduate (e.g., BSc) or postgraduate (e.g., MSc, PhD) student;
  • being a recent undergraduate or postgraduate student (conferral of degree after 1 January of the year preceding the conference) who are presenting their thesis work.

Entering couldn’t be easier! Make sure you nominate yourself when you submit your abstract on-line. You’ll receive a letter, known as ‘Letter of Schedule’, confirming your presentation has been accepted, which will also include a link by which to register for the award. Before the conference, make sure you include the OSPP label (which you can find here) to your PICO presentation header so that the judges of the OSPP award now to evaluate your presentation.

To learn more about PICO presentations see the General Assembly website or download the How to make a PICO guide. For a first-hand account of what it’s like to take part in a PICO session, take a look at this post by early career scientists in the Seismology Division too.  Finally, you can also check out the short introductory video below:

Imaggeo on Mondays: Isolated storm

Imaggeo on Mondays: Isolated storm

Clouds and storms are formed when warm, moist air rises. This causes the air to expand and cool: forming clouds as the moisture condenses onto particles suspended in the air (called cloud condensation nuclei). Normally, air rises from surface heating, or when warm and cold air pockets collide, or if air is pushed upwards when passing over hills or mountains. If this heating, and subsequent rising, is rapid enough then thunderstorms can form.

This imaggeo on Mondays photo shows an isolated thunderstorm roughly 50 km North of Vienna. The difference between an isolated thunderstorm and scattered storms is how much coverage the clouds have over a given area. If less than 10-20 % is covered then these storms are described as isolated. Scattered storms occur when coverage is at least 30-50 %. These storms can lead to downpours lasting a few minutes that then leads to sunny spells, only to have another rain storm occur again shortly afterwards.1

Globally, there are roughly 16 million thunderstorms each year, and at any given moment, there are ~2,000 thunderstorms in progress.2 The visible dark grey anvil shape and the fact that the lighter clouds above appear to be being ‘pulled into’ the storm suggests that this is a ‘severe’ thunderstorm. This means that the storm is self-supporting3 and can cause more extreme impacts than a normal thunderstorm. Rainfall is more intense and can cause flash flooding. In some cases, hail over 2.5 cm large can fall and tornados can even be formed.4 For more information about severe thunderstorms please check out the further reading list below.

By Sarah Connors, EGU Science Policy Officer

Further reading / sources

[1] – Aerostorms Scattered vs. Thunderstorms – http://www.aerostorms.com/scattered-vs-isolated-thunderstorms-what-is-the-difference/

[2] – Thunderstorm Basics – http://www.nssl.noaa.gov/education/svrwx101/thunderstorms/

[3] – Royal Meteorological Society Thunderclouds presentation – http://www.met.reading.ac.uk/~sgs02rpa/CONTED/WEATHER09_thunder.pdf

[4] – Frequently Asked Questions About Thunderstorms – http://www.nssl.noaa.gov/education/svrwx101/thunderstorms/faq/

Imaggeo is the EGU’s online open access geosciences image repository. All geoscientists (and others) can submit their photographs and videos to this repository and, since it is open access, these images can be used for free by scientists for their presentations or publications, by educators and the general public, and some images can even be used freely for commercial purposes. Photographers also retain full rights of use, as Imaggeo images are licensed and distributed by the EGU under a Creative Commons licence. Submit your photos at http://imaggeo.egu.eu/upload/.

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