GeoLog

Natural Hazards

Imaggeo on Mondays: Moving images – Photo Contest 2016

Since 2010, the European Geosciences Union (EGU) has been holding an annual photo competition and exhibit in association with its General Assembly and with Imaggeo – the EGU’s open access image repository.

In addition to the still photographs, imaggeo also accepts moving images – short videos – which are also a part of the annual photo contest. However, 20 or more images have to be submitted to the moving image competition for an award to be granted by the judges.

This year saw seven interesting, beautiful and informative moving images entered into the competition. Despite the entries not meeting the required number of submissions for the best moving image prize to be awarded, three were highly ranked by the photo contest judges. We showcase them in today’s imaggeo on Mondays post and hope they serves as inspiration to encourage you to take short clips for submission to the imaggeo database in the future!


Aerial footage of an explosion at Santiaguito volcano, Guatemala. Credit: Felix von Aulock (distributed via imaggeo.egu.eu)

During a flight over the Caliente dome of Santiaguito volcano to collect images for photogrammetry, this explosion happened. At this distance, you can clearly see the faults along which the explosion initiates, although the little unmanned aerial vehicle is shaken quite a bit by the blast.


Undulatus asperitus clouds over Disko Bay, West Greenland. Credit: Laurence Dyke(distributed via imaggeo.egu.eu)

Timelapse video of Undulatus asperitus clouds over Disko Bay, West Greenland. This rare formation appeared in mid-August at the tail end of a large storm system that brought strong winds and exceptional rainfall. The texture of the cloud base is caused by turbulence as the storm passed over the Greenland Ice Sheet. The status of Undulatus asperitus is currently being reviewed by the World Meteorological Organisation. If accepted, it will be the first new cloud type since 1951. Camera and settings: Sony PMW-EX1, interval recording mode, 1 fps, 1080p. Music: Tycho – A Walk.

Lahar front at Semeru volcano, Indonesia. Credit: Franck Lavigne (distributed via imaggeo.egu.eu)

Progression of the 19 January 2002 lahar front in the Curah Lengkong river, Semeru volcano, Indonesia. Channel is 25 m across. For further information, please contact me (franck.lavigne@univ-paris1.fr)

 

GeoSciences Column: Hazagora – will you survive the next disaster?

GeoSciences Column: Hazagora – will you survive the next disaster?

There is no better thing, on a cold and stormy winter’s evening, than to gather your friends for a night of games / board games. Fire blazing (if you have one), tasty snacks laid out and drinks poured, you are all set to indulge in a night of scheming (if you are playing battle ship), deceit (Cluedo), or even all out comedy (think Pictionary or Charades).

The main purpose of the games you are likely to enjoy, in the relaxed setting described above and in the company of your nearest and dearest, is to entertain. You might not be aware that in playing board games you are also boosting your cognitive, decision-making and social skills. Serious games exploit this notion in order to support learning and raise awareness of important issues, as Dr. Mirjam S. Glessmer previously wrote about in our GeoEd column. With this in mind, could a board game be used to raise awareness about the complexities of geohazards and disaster risk reduction management?

A team of Belgian researchers set out to test the idea by developing Hazagora: will you survive the next disaster? Its effectiveness as an educational tool, both for those living in disaster prone areas, as well as stakeholder and scientists involved in risk management activities, is discussed in a paper recently published in the EGU’s open access journal Natural Hazards and Earth System Sciences.

Playing the game

The game is set on an island, with a central volcano surrounded by forests, agricultural lands and coastal areas. Immerse yourself in the game and you’ll have the option to embody one of five characters: the mayor, the fisherman, the lumberjack, the farmer and the tour guide.  Potential locations where players can settle, with their families, road networks and wells to provide water supply, are drawn on the board game. The board is divided into different sectors which can be affected by a geohazard. The game is led by a game master, bound to follow the Hazagora guidelines.

 Setup of the game: (a) board game; (b) character cards with from left to right: the mayor, the fisherman, the lumberjack, the farmer and the tour guide; (c) resource cards: bread, water and bricks; (d) resource dice; (e) water well and food market; (f) hut (one chip with one family), house (two chips with two families), and road; (g) cost information card for building new streets, huts, and houses and buying protection cards. Taken from Mossoux, S., et al. (2016).

Setup of the game: (a) board game; (b) character cards with from left to right: the mayor, the fisherman, the lumberjack, the farmer and the tour guide; (c) resource cards: bread, water and bricks; (d) resource dice; (e) water well and food market; (f) hut (one chip with one family), house (two chips with two families), and road; (g) cost information card for building new streets, huts, and houses and buying protection cards. Taken from Mossoux, S., et al. (2016).

The outcome of a natural disaster, contrary to common reporting in the media and popular belief, is not exclusively controlled by the force of the natural hazard. The livelihood profile of each of the characters in the game is specifically chosen to highlight the important role economic, social, physical and environmental circumstances play in shaping how individuals and nations are affected by geohazards. A fisherman will inevitably be limited in his choice of settlement location, as he/she is bound to live close to the coast, while at the same time his/her occupation controls its income. On a larger scale, political and socioeconomic factors mean that victims of natural hazards in developing countries, especially Asia and Africa, are more vulnerable to geohazards when compared to residents of developed nations.

Life on the island unfolds in years, with players establishing his/her family on the land by providing shelter, bread (food) and water. Income is received each round table and can be used to a) provide for the family or b) invest in further developing their settlement by adding more housing for extra families. At any given time, and without warning, the game master can introduce a natural hazard (earthquake, tsunami, lava flow, ash fall). All players watch a video clip which illustrates the hazard and outlines the impacts based on recent disasters. The players then discuss the potential damage caused by the hazard to infrastructure, resources and people involved in the game based on factors such as their geographical location relative to the disaster, economic potential and available natural resources. The outcome is displayed on an impact table and the damaged infrastructure removed from the board. Affected families also receive no income during the following roundtable and neighbouring natural resources become contaminated. In this way, the players visually experience complex situations and are able to test new resilience strategies without having to deal with real consequences.

(a) Game session organized with citizens in Moroni (Comoros Islands). (b) Interaction among Belgian students to develop a resilient community. Taken from Mossoux, S., et al. (2016)

(a) Game session organized with citizens in Moroni (Comoros Islands). (b) Interaction among Belgian students to develop a resilient community. Taken from Mossoux, S., et al. (2016)

Players also have the opportunity to acquire protective action cards which can be used to mitigate, prepare or adapt to hazards. The cards can be used by individuals, but also be part of community actions. During a natural hazard, players can decide to use their cards, individually or as a team, to avoid (some) of the impacts caused by the geohazard. This approach stimulates learning about the risks and mitigation strategies associated with natural hazards, by allowing players to test, experience and discuss new management ideas.

The game lasts for a minimum of five years, or equivalent to three hours game time, after which the resilience of the community (which takes into account factors such as number of living families with permanent shelter and access to natural resources) is evaluated using a resilience index. Players are ranked according to their resilience index, thus generating discussion and analysis of strategies which lead to some players fearing better than others.

Following the game, do players better understand natural hazards?

To test the success of the game at raising awareness of natural hazards, the researcher’s carried out a number of game sessions. A total of 21 secondary school and university students from Belgium, as well as a further 54 students, citizens, earth scientist and risk managers from Africa took part in the sessions. Players completed questionnaires before and after the games to evaluate how their understanding of natural hazards and risk management strategies changed after having played Hazagora.

Appreciation of the game by the players (n=75). (∗) Results are significantly different between European and African players (p <0.05). Taken from Mossoux, S., et al. (2016). Click to enlarge.

Appreciation of the game by the players (n=75). (∗) Results are significantly different between European and African players (p <0.05). Taken from Mossoux, S., et al. (2016). Click to enlarge.

The questionnaires revealed that participants found the game fun to play and greatly appreciated the flexibility offered to players to come up with their own adaptation and mitigation strategies. The scientific information regarding the physical processes driving natural hazards was the main thing European players learnt from the game. In contrast, West African players highlighted the usefulness of the game to develop personal and professional mitigation plans; the learning outcomes reflecting the differing life experiences and geological situations of the participants.

Hazagora succeeds in making players more aware of the mechanisms which drive natural hazards and how communities’ vulnerabilities differed based on social-economic factors, rather than depending solely on the potency of the geohazard. By driving discussion and collaboration among players it also stimulates engagement with the importance of disaster risk reduction strategies, while at the same time developing player’s social and negotiation skills. And so, following an enjoyable afternoon of gaming, Hazagora achieves its goal and becomes a great addition to the tools already available when it comes to raising awareness of geohazards.

By Laura Roberts Artal, EGU Communications Officer.

 

References

Mossoux, S., Delcamp, A., Poppe, S., Michellier, C., Canters, F., and Kervyn, M.: Hazagora: will you survive the next disaster? – A serious game to raise awareness about geohazards and disaster risk reduction, Nat. Hazards Earth Syst. Sci., 16, 135-147, doi:10.5194/nhess-16-135-2016, 2016.

Hazagora is a non-commerical game that is available upon request – please contact the study authors for more details.

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.

When mountains collapse…

When mountains collapse…

Jane Qiu, a grantee of the Pulitzer Center on Crisis Reporting, took to quake-stricken Nepal last month — venturing into landslide-riddled terrains and shadowing scientists studying what makes slopes more susceptible to failure after an earthquake. The journey proved to be more perilous than she had expected.

What would it be like to lose all your family overnight? And how would you cope? It’s with these questions in mind that I trekked with a heavy heart along the Langtang Valley, a popular touristic destination in northern Nepal.

Exactly a year ago this week, this remote Himalayan watershed witnessed the single most horrific canastrophy of the Gorkha Earthquake: a massive avalanche engulfed Langtang and nearby villages, leaving nearly 400 people killed or missing.

The quake shook up ice and snow at five locations along a 3-kilometre ridge between 6,800-7,200 metres above sea level. They went into motion and swept huge amounts of loose debris and fractured rocks along their way — before crashing several kilometres down to the valley floor.

The avalanche generated 15 million tonnes of ice and rock, and sent powerful wind blasting down the valley, flattening houses and forests. Wind speeds exceeded 322 kilometres per hour and the impact released half as much energy as the Hiroshima nuclear bomb. Nothing in its path could have survived.

A pile of commemorating stones on the debris that buried Langtang and nearby villages last April, killing and leaving missing nearly 400 people. (Credit: Jane Qiu)

A pile of commemorating stones on the debris that buried Langtang and nearby villages last April, killing and leaving missing nearly 400 people. (Credit: Jane Qiu)

Where the villages used to stand is now a gigantic pile of debris, up to 60 metres deep. It’s effectively a mass grave where people pile up stones and put up prayer flags to mark where their loved ones used to live.

It’s hard to come to terms with the scale of the devastation. Everybody in the valley has lost somebody to the monstrous landslide. About two dozen children from 16 families, who were in schools in Kathmandu during the earthquake, lost all their family in the matter of a few minutes.

It’s a sombre reminder of how dangerous it can be in the Himalayas — where people live so close to ice and where population growth and the search for livelihood often push them to build in hazardous areas.

The only building in the village of Langtang that survived the avalanche. The rocky enclave protected it from the crushing debris and the powerful blast. (Credit: Jane Qiu)

The only building in the village of Langtang that survived the avalanche. The rocky enclave protected it from the crushing debris and the powerful blast. (Credit: Jane Qiu)

Under-appreciated danger

The Langtang tragedy also reminds us how deadly landslides can be during an earthquake — a danger that is often under-appreciated. While earthquakes and landslides are like conjoined twins that go hand in hand, most of the resources go into building houses that can sustain strong shaking, and far too little into mitigating landslide risks.

In both the 2005 magnitude-7.6 Kashmir Earthquake in Pakistan and the 2008 magnitude-7.8 Wenchuan Earthquake in China — which killed approximately 26,000 and 90,000 people, respectively — a third of the fatalities were caused by landslides. While it’s certainly important to build earthquake-proof houses, it’s equally important to build them at safe locations.

In addition to the killer avalanche in Langtang, the Gorkha Earthquake unleashed over 10,000 landslides across Nepal, which blocked rivers and damaged houses, roads, and hydropower stations. Many valleys are totally shattered — with landslide scars running down from the ridge top like gigantic waterfalls, and numerous small failures marring the landscape like fireworks shooting across the sky.

Driving along the Aniko Highway that connects Nepal with Tibet, it’s not difficult to see that many houses had survived the shaking only to be crushed by debris flows and rock falls. The border remains closed because of continuing landslide hazards. The highway, which used to have some of the worst traffic jams in Nepal, is totally deserted.

A building in Kodari — which used to be a bustling trade town at the Nepal-Tibet border — was unscathed during the earthquake only to be damaged by large rock falls. (Credit: Jane Qiu)

A building in Kodari — which used to be a bustling trade town at the Nepal-Tibet border — was unscathed during the earthquake only to be damaged by large rock falls. (Credit: Jane Qiu)

Enduring legacy

A major concern is that Nepal will suffer from more severe landslides than usual for a long time. During the last monsoon, the landslide rate was about ten times greater than an average year. And my trek along the Langtang Valley was accompanied by frequent sound tracks of falling rocks and shifting slopes. A number of times, I had to run from boulders crushing down onto the trail — a clear sign that there are lots of instability in the system.

The instability could go on for years or even decades and will be exacerbated by rainfall and aftershocks. This enduring legacy is often not fully taken on board in quake recovery — with devastating consequences. Eight years after the Wenchuan Earthquake, for instance, settlements built after the disaster continue to be inflicted by a heightened level of landslides, which cause floods and destroy infrastructures.

This points to the importance of rigorous risk assessment before reconstruction and close monitoring afterwards. There is also an urgent need to better understand what makes mountainsides more susceptible to landslides after an earthquake and how they recover over time.

To achieve that end, several research groups went into landslide-ridden areas in Gorkha’s immediate aftermath. They wanted to capture what happened to the landscape immediately after the quake, so they could track the changes in the coming years.

Early warning

Last month, I joined one such team — consisting of Christoff Andermann, Kristen Cook and Camilla Brunello, of the German Research Centre for Geosciences (GFZ) in Potsdam, Germany, and their Nepalese coordinator Bhairab Sitaula — on a field trip along the Arniko Highway.

That was their fourth trip in Nepal since last June when they began to map the landslides and installed a dozen broadband seismometers, along with weather stations and river-flow sensors, over 50 square kilometres of badly shaken terrains.

The team often attracted a few curious onlookers when they worked away, but nothing provoked more excitement than the drone, says Cook. The crowd, especially kids, were thrilled to see the little robotic device buzzing around like a gigantic mosquito, she adds. A camera and sensors onboard can help them to locate the landslides and monitor debris movement, especially after rainstorms.

 

Christoff Andermann, Camilla Brunello and Bhairab Sitaula performing maintenance on a broadband seismometer and weather station near the village of Chaku on the Arniko Highway (Credit: Jane Qiu)

Christoff Andermann, Camilla Brunello and Bhairab Sitaula performing maintenance on a broadband seismometer and weather station near the village of Chaku on the Arniko Highway (Credit: Jane Qiu)

Another exciting aspect of their research is the use of seismology to probe geomorphic processes over a large area. Landslides are effectively earthquakes that occur near the surface, and produce signals that can be picked up by seismometers.

The team, led by Niels Hovius of GFZ, can detect precursory seismic signals days before a landslide happens. They also study ground properties by measuring how traffic vibrations travel through the ground.

Because seismic waves travel faster when subsurface materials are wet, the researchers are able to trace how rainfall penetrates into and through the ground. This determines the pressure of water in spaces between soil and rock particles, a key factor controlling slope stability.

Such studies will one day allow researchers to determine the rainfall thresholds that could precipitate a landslide and capture deformation precursors days in advance. This offers a real prospect of an effective early warning system, which is urgently needed in a country that is increasingly plagued by landslides.

By Jane Qiu, freelance science writer in Beijing

Further reading

Qiu, J. Listening for landslides, Nature 532, 428-431 (2016).

Jane Qiu, an awardee of the 2012 EGU Science Journalism Fellowship, is a Chinese freelance science writer in Beijing. She is passionate about the origin and evolution of the Tibetan Plateau and surrounding mountain ranges—a vast elevated land also known as the Third Pole because it boasts the largest stock of ice outside the Arctic and the Antarctic. 

Travelling extensively across the Third Pole, up to 6,700 meters above sea level (http://science.sciencemag.org/content/351/6272/436), Qiu has covered wide-ranging topics—from the meltdown of Himalayan glaciers, grassland degradation, the origin of woolly rhino, to the people of Tibet. Her work regularly appears in publications such as Nature, Science, The Economist, Scientific American, and SciDev.Net.

Qiu’s journey to the Third Pole began with Marine Biological Laboratory’s Logan Science Journalism Fellowship that allowed her to travel to the Arctic and the Antarctic and report climate change first hand. These experiences sowed the seeds for her later fascination with geoscience and environmental studies, and afforded her the insight to draw parallels between these geographically diverse regions.

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