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Blogs and social media at the Assembly – tune in to the conference action

23 Apr

Blogging

GeoLog will be updated regularly throughout the General Assembly, highlighting some of the meeting’s most interesting sessions, workshops and lectures, as well as featuring interviews with scientists attending the Assembly.

Writers from the EGU Blog Network will also be posting about interesting research and sessions during the Assembly, so you can catch up on any sessions you’ve missed and get a feel for what’s going on in the press room through them!

As in previous years, the EGU will be compiling a list of General Assembly related blogs (the blogroll) and making them available through GeoLog. If you would like to contribute to GeoLog during the event please contact Sara Mynott at mynott@egu.eu. You can also add your blog to the blogroll here.

EGU social media

Tweeting

Participants can keep updated with General Assembly goings on by following the EGU twitter account (@EuroGeosciences) and the conference hashtag (#EGU2014). You can also direct questions to the EGU communications staff and other participants using #EGU2014, or by tweeting to @EuroGeosciences directly. If you’ve got the Assembly app, you can share snippets of great sessions straight from there!

This year, each of the programme groups also has its own hashtag, if you’re in a Geomorphology (GM) session, say GM2.1, you can tweet about it using #EGU14GM, or if you’re in one of the Educational and Outreach Symposia (EOS), use #EGU14EOS – just add the acronym to #EGU14! A full list of conference hashtags is available here, and in the programme book.

Some sessions also have their own hashtag including the Great Debates (GDB1#EGU14mine, GDB2: #EGU14geng), the Union Session on the IPCC results (US4: #EGU14IPCC) and the Face of the Earth Union Symposium (US3: #EGU14face). Make sure to tag your tweets accordingly if you are posting about these sessions! Conveners are welcome to add their own hashtags into the mix to! Just let everyone know at the start of the session.

The view from social media HQ at EGU 2012.

The view from social media HQ at EGU 2012.

And more!

While these will be the main media streams during the Assembly, you can also follow the European Geosciences Union on FacebookGoogle+LinkedIn and YouTube to keep up with us there!

Video Competition finalists – time to get voting!

15 Apr

This year we’re running the first ever EGU Communicate Your Science Video Competition – the aim being for young scientists to communicate their research in a short, sweet and public-friendly video. Our judges have now selected 4 fantastic finalists from the excellent entries we received this year and it’s time to find the best geoscience communication clip!

The shortlisted videos will be open to a public vote from now until midnight on 1 May – just ‘like’ the video on YouTube to give it your seal of approval. The video with the most likes when voting closes will be awarded a free registration to the EGU General Assembly 2015.

The finalists are shown below, but you can also catch them in this finalist playlist and even take a seat in GeoCinema – the home of geoscience films at the General Assembly – to see the shortlist and select your favourite.

Please note that only positive votes will be taken into account.

The finalists:

Into the Iron Zone by Carolina Reyes. Like this video to vote for it!

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Understanding Ice-Sheet Stability Using Rocks by Richard Jones. Like this video to vote for it!

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Hydrological Drought Predictions for Reservoir Management: What’s the Use? by Louise Crochemore. Like this video to vote for it!

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SLOMOVE by Giulia Chinellato. Like this video to vote for it!

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The winning entry will be announced during the lunch break on the last day of the General Assembly (Friday 2 May).

Sci Comm at the 2013 General Assembly

27 Mar

Blogging

GeoLog will be updated regularly throughout the General Assembly, highlighting some of the meeting’s most interesting sessions, workshops and lectures as well as featuring interviews with scientists attending the Assembly.

Writers from the EGU Blog Network will also be posting about interesting research and sessions during the Assembly, so you can catch up on any sessions you’ve missed and get a feel for what’s going on in the press room through them!

As in previous years, the EGU will be compiling a list of General Assembly related blogs (the blogroll) and making them available through GeoLog.  If you would like to contribute to GeoLog, add your blog to the blogroll, or join the EGU Blog Network please contact Sara Mynott at mynott@egu.eu.

Tweeting

Participants can keep updated with General Assembly goings on by following the EGU twitter account (@EuroGeosciences) and the conference hashtag (#egu2013). You can also direct questions to the EGU communications staff and other participants using #egu2013, or by tweeting to @EuroGeosciences directly.

Some sessions also have their own hashtag including the Great Debate (GDB1; #eguFrack), the Union Session on Curiosity (US2; #eguMars), how to apply for a job (SC9/EOS13;#eguJobs), and how to use blogs and social media in scientific research (SC8/EOS12; #eguSMedia). Make sure to tag your tweets accordingly if you are posting about these sessions!

 

And other social media!

While these will be the main media streams during the Assembly, you can also follow the European Geosciences Union on Facebook, Google+, LinkedIn and YouTube to keep up with us there!

Using social networks to respond to earthquakes

21 Feb

Effective responses to natural disasters require the rapid acquisition of information about where has been affected, how many people are in the affected areas and what the magnitude of the damage is. This information is critical in both disaster and emergency rescue management. Indeed, the first three days after the onset of a disaster has been dubbed the “72-hour golden rescue period”, after which the survival rate of victims sharply declines. With this in mind, the need for rapid data collection could not be more evident.

Aerial photography is a useful tool in determining which areas have been affected by an earthquake, but resolution may not always be adequate to determine the damage to buildings and infrastructure within them. For this, satellite technology provides a helping hand. For example, the spectral characteristics of a building can be used to determine whether or not it has been structurally damaged. There is, however, a time delay associated with gathering and analysing satellite data and it is ineffective for more minor quakes. More importantly though, these tools provide no indication of the number of people affected within these areas beyond the assumed population density (affected rural land is likely to have fewer people immediately at risk than in an affected urban area).

Building collapse as a result of the 1995 Hanshin-Awaji earthquake [Source: Wikimedia Commons].

So what options do we have for gathering this information in semi-real time (within the golden rescue period)? If mobile phone communications are not affected, information sent via text messages can provide fundamental support for search and rescue teams. Currently, the China Earthquake Administration has a platform designed to receive short text and voicemail messages about disasters using the number 12322. The problem lies in the rapid extraction of the most relevant details from these messages, so that useful information can be disseminated to people on the ground.

This is where Dr Jing Hai Xu and his team come in, as they have developed a method of using text messages to report and disseminate disaster information and Geographic Information Systems (GIS) to analyse and extract details relevant to search and rescue teams.

The network is separated into country level, provincial level, and city level, with the smallest components being streets within a town or city. One reporter is enough to include the impact on a particular location in the disaster information network. One downside of the model, though, is that the reporters need to be formal local government employees. Whilst this measure is proposed to increase the reliability of reports, it vastly reduces the number of people that can feed into the network. Perhaps an alternative way of addressing the problem of reliability would be to only include information in the network after multiple reports of a similar incident are received from the same area. Here we are faced with new problems: what constitutes one area? Will reports of the same event from different observers be sufficiently similar to be picked up in the network? This also requires the contact details of the disaster network to be disseminated to a greater proportion of the population… perhaps Xu et al.’s approach is an effective one after all!

Now that that’s decided – how does it work? Principally, there are two kinds of nodes that help the network function: 1) edge nodes, these are the people responsible for reporting disaster information, and 2) central nodes, which correspond to the central earthquake office within each city and are responsible for collecting and disseminating information. After an earthquake, the city earthquake office (central node) contacts the reporters (edge nodes), asking for information about the impact of the disaster where they are. This information is fed back to the office and these central nodes pass the information on to the provincial offices and then on to the country’s government office so that appropriate action can be taken.

Having a simple code for different impacts helps collate useful information. In this model, the first number indicates the type of damage (e.g. 4 for damage to buildings) and the second indicates the severity (with 1 being low severity and 5 being high). So the code for a few damaged buildings would be 42, or 44 for a large quantity of damaged buildings, with some partially collapsed, etc. Here are the other codes:

Earthquake disaster information codes (click to enlarge), [modified from Xu et al., 2013].

The collected information can then be displayed using GIS, a visual mapping program, which will regularly update to incorporate new reports and can be used to effectively inform search and rescue teams. Again, this can be achieved through sending text messages to relay disaster information to teams that are out on site.

Disaster information distribution (level of shaking) from the 2012 Yangzhou earthquake, [modified from Xu et al., 2013].

The only question remaining is how can we manage sending and receiving so many messages? There are 1048 reporters in the Changzhou network alone and handling a volume of messages this large requires something called a mobile agent server (MAS). A MAS is capable of sending nearly 100 messages per second – efficient enough to rapidly collate information following an earthquake and let officials take action. The 150 data principle (part of social network theory) is relevant here. This principle is based on the idea that people cannot stably maintain networks of more than 150 people; for the same reason, disaster management isn’t effective when there are more than 150 people in a network. Thus, reporters in the Changzhou network are subdivided to better relay information about the impacts of earthquakes on local people, buildings and infrastructure.

So there you have it – the key to disaster management success: send an SMS.

By Sara Mynott

Reference:

Xu, J. H., Nie, G. Z., and Xu, X.: A digital social network for rapid collection of earthquake disaster information, Nat. Hazards Earth Syst. Sci., 13, 385-394, doi:10.5194/nhess-13-385-2013, 2013

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