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Share the work you presented at EGU 2016: upload your presentations for online publication

Share the work you presented at EGU 2016: upload your presentations for online publication

This year it is, once again, possible to upload your oral presentations, PICO presentations and posters from EGU 2016 for online publication alongside your abstract, giving all participants a chance to revisit your contribution  hurrah for open science!

Files can be in either PowerPoint or PDF format. Note that presentations will be distributed under the Creative Commons Attribution 3.0 Licence. Uploading your presentation is free of charge and is not followed by a review process. The upload form for your presentation, together with further information on the licence it will be distributed under, is available here. You will need to log in using your Copernicus Office User ID (using the ID of the Corresponding Author) to upload your presentation.

Presentations and posters will be linked to from their corresponding abstracts. If your presentation didn’t have an abstract (this is the case for Short Courses and others), but you still want to share it with the wider community you can consider uploading your presentation to slideshare or figshare as a PDF to share it instead.

All legal and technical information, as well as the upload form, is available until 19 June 2016 at: http://meetingorganizer.copernicus.org/egu2016/abstractpresentation

Geo Talk: One of the youngest EGU 2016 General Assembly delegates sends sensor to space

Geo Talk: One of the youngest EGU 2016 General Assembly delegates sends sensor to space

Presenting at an international conference is daunting, even for the most seasoned of scientists; not so for Thomas Maier (a second year university student) who took his research (co-authored by  Lukas Kamm, a high-school student) to the EGU 2016 General Assembly! Not only was their work on developing a moisture sensor impressive, so was Thomas’ enthusiasm and confidence when presenting his research. Hazel Gibson and Kai Boggild, EGU Press Assistants at the conference, caught up with the budding researcher to learn more about the pair’s work. Scroll down to the end of this post for a full video interview with Thomas. 

Thomas Maier might seem like your average bright and enthusiastic EGU delegate, but together with his co-author Lukas Kamm, he has invented a water sensor that very well might help change the way astronauts live in space. Not only is their invention helping to revolutionise aerospace, but they are also the youngest delegates at the conference, Thomas is a second year university student at Friedrich-Alexander Universität Erlangen-Nürnberg and Lukas is attending high school at Werner-von-Siemens Gymnasium. We caught up with Thomas to speak with him about his invention.

Could you explain to us what led you to develop this water sensor?

We started this project four years ago for a contest called Jugend Forscht, a German youth sciences competition in Germany and the project we came up with was about giving plants demand driven watering. After we built our first sensor, we continued our work until it was possible to send the sensor into space, for a project called EU:CROPIS.

Can you tell us how your sensor works?

The sensor is based on a capacitive measuring method. So, you have two electrodes close to each other, which have an electrical capacitance (or ability to store an electrical charge) between them. The change in water content close to the electrodes changes the capacity of the sensor. Then we measure the capacity of the electrodes by measuring the time constant of the capacitor over time.

The greenhouse which forms part of the EU:CROPIS project. The greenhouse is home to Thomas and Lukas' water sensor. (Credit: Kai Boggild/EGU)

The greenhouse which forms part of the EU:CROPIS project. The greenhouse is home to Thomas and Lukas’ water sensor. (Credit: Kai Boggild/EGU)

Can you tell us more about the EU:CROPIS project?

The EU:CROPIS is mainly about this here [indicates greenhouse model], and this is a greenhouse which will go into space, July next year. The greenhouse will rotate and will generate different gravitational forces that may impact the amount of water available to plants which will be grown in here. And now, after a lot of work, our sensor will be placed on the very right [hand side] of the greenhouse and will measure the soil moisture for the plants.

What are you plans for this project into the future?

Our plans for the future are in taking part in the EDEN-ISS project, this is a project on the International Space Station, that is looking into planting 20 square meters of plants in the ISS and our sensor would be used too. So that is the next aim of this project.

Thanks Thomas for showing us your invention, and good luck to Lukas, who couldn’t attend the conference this year as he is busy with his high-school exams!

Interview by Hazel Gibson, video interview by Kai Boggild, EGU Press Assistants

 

GeoPolicy: How to communicate science to policy officials – tips and tricks from the experts

GeoPolicy: How to communicate science to policy officials – tips and tricks from the experts

The EGU General Assembly was bigger than ever this year. Over 16,500 people attended more than 500 sessions. Although many sessions featured policy-relevant science, the short course entitled ‘Working at the science policy interface‘ focused purely on the role of scientists within the policy landscape. For those of you that couldn’t attend, this month’s GeoPolicy post takes a closer look at what was discussed.

The short course consisted of three panellists; Katja Rosenbohm, Head of Communications at the European Environment Agency (EEA), Panos Panagos, Senior Research Scientist in the Land Resource Unit at the European Commission’s Joint Research Centre (JRC), and Valérie Masson-Delmotte, Head of the IPCC AR6 Working Group 1 (IPCC). Each speaker gave a short presentation, introducing their respective institutions  and how their work connects science to policy. The session concluded with questions taken from the audience. EGU Press Assistant, Hazel Gibson (@iamhazelgibson), live-tweeted the session and a Storify of the tweets can be found here.

 

Katja Rosenbohm & the EEA: assessing if the EU is achieving its policy goals 

The European Environment Agency (EEA) provides independent information on the environment to European and national level policy makers, as well as to the general public. Katja spoke of the EEA’s State of the Environment Reports which are published every 5 years. These reports give ‘a comprehensive assessment of the European environment’s state, trends and prospects, in a global context’ and include analysis of 11 global megatrends, 9 cross-country comparisons, and 25 European environmental briefings. These reports help the EU analyse whether current policy is achieving their desired goals.

The 2015 State of the Environment Report concludes with 4 key messages:

  • Policies have delivered substantial benefits for the environment, economy and people’s well-being; major challenges remain
  • Europe faces persistent and emerging challenges linked to production and consumption systems, and the rapidly changing global context
  • Achieving the 2050 vision requires system transitions, driven by more ambitious actions on policy, knowledge, investments and innovation
  • Doing so presents major opportunities to boost Europe’s economy and employment and put Europe at the frontier of science and innovation

A copy of Katja’s slides can be found here.

 

Panos Panagos & the JRC: the policy cycle & communicating your research

Panos introduced the JRC, the European Commission’s in-house research centre. The JRC has a near-unique position in which all its research directly provides scientific and technical support to policy. As a result, all research at the JRC tries to solve the societal challenges of our time, i.e. food security, energy resources, climate change, innovation and growth etc. Panos explained that scientific evidence can be used to assist policy at all stages of the ‘policy cycle’ (see figure below) but scientists must learn how to present their research so that policy officials can understand.

The Policy Cycle and where scientific evidence can be used. Slide taken from Panos Panagos' talk. Full presentation can be foudn here.

The Policy Cycle and where scientific evidence can be used. Slde taken from Panos Panagos’ talk. Full presentation can be found here.

Factors needed for scientific evidence to inform policy:

  • TRUST because if there is no trust, the evidence will be ignored
  • TIMING / RELEVANCE is vital and should be provided as early as possible in the policy cycle. The speed of scientific response after a specific event is crucial – evidence can be submitted too late, after a policy decision has been made.
  • FORM should not be a 500 page report. It should be concise. Policy makers do not have time to read long reports or interpret data.
  • FORMAT provide policymakers with concise, visual input so that they can quickly understand the main messages – graphs should have a maximum of 3 colours!
  • PRACTICE the science-policy relationship needs to move from being a formal, arms-length, linear relationship, to an iterative one where questions and answers are generated through co-creation by both scientists and policymakers

A copy of Panos’ slides can be found here where you can learn more about the JRC and the projects they have been involved with.

 

Valérie Masson-Delmotte & the IPCC: what’s next after COP21?

Valérie spoke of the IPCC and how these reports inform world leaders and policy officials about climate change. The IPCC is split into three Working Groups (WG):

  • WG1: understanding the scientific basis of risk of human-induced climate change;
  • WG2: its potential impacts
  • WG3: options for adaptation and mitigation.

Last year, Valérie was appointed co-chair of the WG1 for the next set of IPCC reports (AR6) which will be published in 2022/3. In her talk, Valérie stressed that ‘the IPCC should be policy relevant but not policy proscriptive’. Scientists should not over-step their mark and become advocates of their research, they must remain unbiased and present their research professionally.

Scientists can indirectly assist policy by contributing to these IPCC reports; either through their academic papers or by becoming co-authors or editors. Three more-focused special reports will be published over the next few years. These are:

  • In the context of the Paris Agreement, special report in 2018 on the impacts of global warming of 1.5°C above pre-industrial levels and related global greenhouse gas emission pathways;
  • A special report on climate change and oceans and the cryosphere;
  • A special report on climate change, desertification, land degradation, sustainable land management, food security, and greenhouse fluxes in terrestrial ecosystems, considering challenges and opportunities both for adaptation and mitigation.

In addition a methodological report on greenhouse gas inventories has also be scheduled for early 2019.

If you can communicate your science to high school students, you are at the right level for policy makers!

When asked about how scientists should communicate their research to policy officials, Valérie suggested that scientists ‘practice’ communicating with teenagers. A 15 year old will quickly tell you if you are making sense or not and you will be able to clarify your meaning.

A copy of Valérie’s slides can be found here.

 

Discussions

The session concluded with a panel discussion and audience members were invited to ask questions. General themes encompassed science communication, science funding, and the division between science and politics.

A couple of the Q&As are listed below.

  • Is there a lack of knowledge in scientists about policy and how can we change that?

Yes but this can be reduced through the creation of networks and collaborations to encourage increasing participation from scientists to policy (bottom up communications). Perhaps an early career scientist and policy worker pairing scheme could help engagement soon rather than later?

  • Is there a fundamental problem with politicians being more accountable to financial interests than good science?

Politicians can use any excuse to get rid of something costly and research is expensive. It is the role of the scientist to explain the value of our research to stop this from happening.

Further discussions are covered in the Storify post created from this session. More general information about science policy can be found on the EGU policy resources website: http://www.egu.eu/policy/resources/

GeoTalk: A smart way to map earthquake impact

GeoTalk: A smart way to map earthquake impact

Last week at the 2016 General Assembly Sara, one of the EGU’s press assistants, had the opportunity to speak to Koen Van Noten about his research into how crowdsourcing can be used to find out more about where earthquakes have the biggest impact at the surface.

Firstly, can you tell me a little about yourself?

I did a PhD in structural geology at KULeuven and, after I finished, I started to work at the Royal Observatory of Belgium. What I do now is try to understand when people feel an earthquake, why they can feel it, how far away from the source they can feel it, if local geology affects the way people feel it and what the dynamics behind it all are.

How do you gather this information?

People can go online and fill in a ‘Did You Feel It?’ questionnaire about their experience. In the US it’s well organised because the USGS manages this system in whole of the US. In Europe we have so many institutions, so many countries, so many languages that almost every nation has its own questionnaire and sometimes there are many inquiries in only one country. This is good locally because information about a local earthquake is provided in the language of that country, but if you have a larger one that crosses all the borders of different countries then you have a problem. Earthquakes don’t stop at political borders; you have to somehow merge all the enquiries. That’s what I’m trying to do now.

European institutes that provide an online "Did You Feel the Earthquake?" inquiry. (Credit: Koen Van Noten)

European institutes that provide an online “Did You Feel the Earthquake?” inquiry. (Credit: Koen Van Noten)

There are lots of these databases around the world, how do you combine them to create something meaningful?

You first have to ask the different institutions if you can use their datasets, that’s crucial – am I allowed to work on it? And then find a method to merge all this information so that you can do science with it.

You have institutions that capture global data and also local networks. They have slightly different questions but the science behind them is very similar. The questions are quite specific, for instance “were you in a moving vehicle?” If you answer yes then of course the intensity of the earthquake has to be larger than one felt by somebody who was just standing outside doing nothing and barely felt the earthquake. You can work out that the first guy was really close to the epicentre and the other guy was probably very far, or that the earthquake wasn’t very big.

Usually intensities are shown in community maps. To merge all answers of all institutes, I avoid the inhomogeneous community maps. Instead I use 100 km2 grid cell maps and assign an intensity to every grid cell.. This makes the felt effect easy to read and allows you to plot data without giving away personal details of any people that responded. Institutes do not always provide a detailed location, but in a grid cell the precise location doesn’t matter. It’s a solution to the problem of merging databases within Europe and also globally.

Underlying geology can have a huge impact on how an earthquake is felt.  Credit: Koen Van Noten.

Underlying geology can have a huge impact on how an earthquake is felt. 2011 Goch ML 4.3 earthquake.  Credit: Koen Van Noten.

What information can you gain from using these devices?

If you make this graph for a few earthquakes, you can map the decay in shaking intensity in a certain region. I’m trying to understand how the local geology affects these kinds of maps. Somebody living on thick pile of sands, several kilometres above the hypocentre, won’t feel it because the sands will attenuate the earthquake. They are safe from it. However, if they’re directly on the bedrock, but further from the epicentre, they may still feel it because the seismic waves propagate fast through bedrock and aren’t attenuated.

What’s more, you can compare recent earthquakes with ones that happened 200 years ago at the same place. Historical seismologists map earthquake effects that happened years ago from a time when no instrumentation existed, purely based on old personal reports and journal papers. Of course the amount of data points isn’t as dense as now, but even that works.

Can questionnaires be used as a substitute for more advanced methods in areas that are poorly monitored?

Every person is a seismometer. In poorly instrumented regions it’s the perfect way to map an earthquake. The only thing it depends on is population density. For Europe it’s fine, you have a lot of cities, but you can have problems in places that aren’t so densely populated.

Can you use your method to disseminate information as well as gather it, say for education?

The more answers you get, the better the map will be. Intensity maps are easier to understand by communities and the media because they show the distribution of how people felt it, rather than a seismogram, which can be difficult to interpret.

What advice would you give to another researcher wanting to use crowd-sourced information in their research?

First get the word out. Because it’s crowd-sourced, they need to be warned that it does exist. Test your system before you go online, make sure you know what’s out there first and collaborate. Collaborating across borders is the most important thing to do.

Interview by Sara Mynott, EGU Press Assistant and PhD student at Plymouth University.

Koen presented his work at the EGU General Assembly in Vienna. Find out more about it here.

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