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- 7 - Earth Systems and Environmental Sciences
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- University of Cambridge
- Unit of assessment
- 7 - Earth Systems and Environmental Sciences
- Summary impact type
- Technological
- Is this case study continued from a case study submitted in 2014?
- No
1. Summary of the impact
University of Cambridge research has focussed on earthquake hazard, risk and resilience, particularly in developing nations along the earthquake belt from the Mediterranean to China. The impact of this research has been:
- To increase the resilience of developing countries to earthquake risk through the foundation (by Jackson) of the international partnership Earthquakes without Frontiers (EwF) which has:
Led to the retrofitting of buildings and development of new building codes, resulting in safer and more resilient buildings;
Improved hazard assessment and city development planning, thereby reducing earthquake risk;
Empowered in-country scientists, leading to improved public safety policy and a shift in the political understanding of managing earthquake risk.
The population exposed to earthquake hazard in the 11 different countries in which EwF is active is 1 billion.
- To allow safer and more cost-effective hydrocarbon exploration as a result of improved assessment of seismic hazard and risk in the Caspian region, an area which has attracted >USD 50 billion of investment but which is at extreme risk of earthquakes.
2. Underpinning research
Jackson’s, Copley’s and Priestley’s research, based on a wide range of geological and geophysical techniques, has underpinned our understanding of how continents deform [R1, 2, 3]. Their studies of fault rupture have led to a quantitative understanding of the hazard that earthquakes pose in continental regions away from tectonic plate boundaries: why they occur, what controls their size and recurrence rate, why people tend to live in areas prone to large earthquakes and what factors control the vulnerability of populations to these hazards.
Cambridge research has shown that seismic risk is higher in continental interiors, where the network of faults is much less well defined, than at plate boundaries [R4]. Since 1900, there have been approximately 130 earthquakes in which >1,000 people died. 100 of these took place in continental interiors causing at least 1,400,000 deaths, compared to 800,000 at plate boundaries. Devastating earthquakes such as those in Bam, Iran (2003; 30,000 deaths), Muzzafarabad, Pakistan (2005; 75,000 deaths) and Wenchuan, China (2008; 70,000 deaths), invariably take place on faults that were either previously unknown, or whose threat had not been recognised [R4], making hazard assessment and development planning impossible.
Cambridge research identified a disparity in the impacts of earthquakes of similar magnitudes between vulnerable developing countries and richer nations; and the complex reasons behind it [R5]. A 7.8 magnitude earthquake could kill up to 30 per million people in California, but up to 10,000 in parts of Asia (U.S. Geological Survey). Historically, population centres in Central Asia sprung up in geologically-rich areas close to water sources and mountain ridges used as trade routes; all features intimately linked to the presence of active faults. For centuries, in countries like Iran, settlements have been destroyed by earthquakes, rebuilt and resettled. Such settlements are now experiencing rapid population growth and urban development. Buildings are of a low quality and have not been managed through building codes [R4, 5]. Earthquakes in these areas will now kill tens or hundreds of thousands as people migrate into megacities in vulnerable locations and it is expected that 2 billion people will be added to the cities of developing nations over the next twenty years. The situation is similar throughout much of the Mediterranean-Middle East-Central Asia earthquake belt. In contrast, in California and Japan, with good building design codes, earthquakes are now principally stories of economic loss [R5].
These multiple findings have been applied by leveraging a long-term relationship built up by Jackson and Copley (and Philip England from the University of Oxford) with local collaborators across the Mediterranean-Himalayan-Asian earthquake belt, many of whom advise their respective governments on earthquake hazard and risk. This created the opportunity to establish the Earthquakes without Frontiers (EwF) project, 2012-2018. Jackson (with England) is the co-founder and co-lead PI on EwF, a joint NERC-ESRC consortium supporting physical and social scientists working to increase resilience to earthquakes in Asian countries. EwF aimed to increase resilience to earthquakes in vulnerable countries through (a) collaborative research to improve knowledge of the hazard; (b) translation of that knowledge into improved public safety; (c) increasing in-country capability through training in modern earthquake science. Countries involved in EwF include Italy, Albania, Greece, Turkey, Iran, Turkmenistan, Kyrgyzstan, Kazakhstan, India, Nepal and China. The population exposed to earthquake in the 11 different countries in which EwF is active is 1 billion. Jackson received a CBE in 2015 for his work in this area.
Cambridge research has also yielded insight into how earthquakes in the south Caspian Sea, and in Iran, Azerbaijan and Turkmenistan, relate to geology and tectonics [R6]. The area is one of prodigious hydrocarbon reserves, with huge investment by oil companies but extreme risk from earthquakes and over-pressured sub-surface fluids, which threaten and frequently damage industry infrastructure through blow-outs and liquefaction. Cambridge research has identified that the simple patterns of earthquake mechanisms which hold the key to the tectonics of the South Caspian region are not clear in the routinely reported earthquake bulletin data, mainly because of errors in focal depths. Those patterns are, however, clear when the focal mechanisms and depths have been improved by long-period waveform modelling [R6]. Cambridge research in the Caspian Sea therefore addresses and corrects these inadequacies, leading to requests for advice from the engineering and oil industries.
3. References to the research
The following papers are peer-reviewed and published in high quality Earth Science journals. The papers are recognised internationally in terms of originality, significance and rigour, as evidenced by their citations and grant funding.
2002 Jackson J. Faulting, flow, and the strength of the continental lithosphere. International Geology Review. 2002 Jan 1;44(1):39-61. doi.org/10.2747/0020-6814.44.1.39
2012 Craig, T.J, Copley, A. & Jackson, J. Thermal and tectonic consequences of India under-thrusting Tibet. Earth & Planet. Sci. Lett., 353-354, 231-239. doi.org/10.1016/j.epsl.2012.07.010
2006 Copley, A. & Jackson, J. Active tectonics of the Turkish-Iranian plateau, Tectonics, 25, TC6006. doi.org/10.1029/2005TC001906
2016 Talebian, M., A. Copley, M. Fattahi, M. Ghorashi, J. Jackson, H. Nazari, R.A. Sloan, R.T. Walker, Active faulting within a megacity: the geometry and slip rate of the Pardisan thrust in central Tehran, Iran, Geophysical Journal International, 207, 3, 1688-1699, doi.org/10.1093/gji/ggw347
2006 Jackson, J. Fatal attraction: living with earthquakes, the growth of villages into megacities, and earthquake vulnerability in the modern world. Phil. Trans. Roy. Soc. London, Ser. A, 364, 1911-1925. doi.org/10.1098/rsta.2006.1805
2002 Jackson, J.A., Priestley, K., Allen, M. & Berberian, M. Active tectonics of the South Caspian Basin. Geophys. J. Int., 148, 214-245. doi.org/10.1046/j.1365-246X.2002.01005.x
Grants (Jackson as PI)
NERC
International Partnership for Collaboration and Training in Earthquake Hazard Assessment and Mitigation in the Alpine-Himalayan Belt and Central Asia. International Opportunities Fund (incl. enhancement) 1.7.2012-28.2.2017 GBP233,407
Earthquakes Without Frontiers: Increasing resilience to Natural Hazards programme (incl. Newton Fund enhancement and supplement for hire of seismic equipment to monitor aftershocks of 2015 Nepal earthquake). 1.7.2012-31.7.2018 GBP737,348
Active tectonics and seismic hazard assessment in Shaanxi, Gansu, and Ningxia Provinces, China. Increasing Resilience to Natural Hazards in China programme. 25.1.2016-24.1.2019 GBP34,022
Shell
- Earthquakes and tsunamis in the Eastern Mediterranean. 1.10.2013-30.9.2017 GBP101,909
DFID
- Rapid release of resources for seismic monitoring in Nepal. 201884. Science for Humanitarian Aid and Resilience programme 2.5.2015-30.9.2017 GBP275,000
Royal Society
- Increasing resilience to earthquakes in North India. ICA\R1\180234 International Collaboration Agreement/GCRF programme. 1.12.2018-30.1.2022 GBP159,250
Grants (Jackson as Co-I)
Leverhulme Trust
- Earthquake Ruptures Of Iran and Central Asia 1.3.2019-28.2.2021 GBP359,347
4. Details of the impact
It is estimated that by 2050, 2 billion people in developing nations will be exposed to serious earthquake risk [E1]. University of Cambridge research, and the co-founding by Jackson of Earthquakes without Frontiers (EwF), has increased the resilience of developing nations to earthquake risk through the retrofitting of buildings and the development of improved building codes; improved hazard assessment and city development planning; and a shift in the political understanding of managing earthquake risk which is the result of the empowerment of local scientists and has led to improved public safety policy. Cambridge research in the South Caspian sea region has also led to safer and more cost effective hydrocarbon exploration.
Retrofitting of buildings and development of new building code has led to safer and more resilient buildings
In the 2015 earthquake in Nepal, 98% of the nearly 9,000 deaths were caused by collapsing buildings. In Kathmandu, 300 buildings retrofitted to increase earthquake resilience by the National Society of Earthquake Technology (NSET) all survived [E2]. NSET attributed their success in securing and delivering construction contracts in Nepal, both before and after the earthquake, to their collaboration with EwF: ‘EwF definitely did help raise the trust of many bi-lateral agencies and other partners on NSET and our approaches, which we could refine and polish due to our association in EwF’ [E2].
Following the earthquake in Nepal, key findings relating to impact and resilience from Jackson and colleagues were presented to DFID, UNESCO and the Nepalese government. These reports were, as the UK government Chief Scientist explained, ‘highly valued by the [FCO and DFID] for use in their operational planning’ [E3]. The Nepalese government used these reports to guide a new building code to improve earthquake resilience. Amongst the organisations awarded contracts for re-building work following the 2015 earthquake in Nepal were the EwF-affiliated NSET, who have been awarded a USD 10 million contract by USAID for the rebuilding of more than 50,000 residential properties and thousands of schools [E2]. The new building code is being used to guide the construction of new schools that are earthquake-resistant, thereby greatly reducing the risk of building collapse and death, and allowing children to attend school without fear.
Improved hazard assessment and planning reduces risks from earthquakes
Cambridge research showed that devastating earthquakes almost invariably take place on faults that were either previously unknown, or whose threat had not been recognised. In Asia there are thousands of active faults which could slip to cause an earthquake at any time, not all of which have been identified. In Tehran – a city of over 10 million people – EwF has addressed this problem by identifying the Pardisan fault, thereby improving hazard assessment and subsequently changing planning policy. The Geological Survey of Iran states that: ‘Collaborations through EwF have provided the possibility of identifying major hidden … faults ... [for example] … identifying and studying the active hidden Pardisan fault within the capital city of Tehran which was a major step in evaluating the earthquake hazard to Tehran’ [E4]. On the back of the University of Cambridge EwF assessment, the Iranian government ‘decided to revise the city development plan considering the new findings’ [E4].
Empowerment of in-country scientists leads to improved public safety policy
Prior to EwF, the predominant view in developing nations was that earthquakes are predictable, so governments needed only to demand short-term predictions from scientists. A system had evolved in which (a) no action was taken on mitigation; (b) maps of seismic hazard were decades old and largely incorrect; and (c) research in modern or innovative directions was rarely encouraged [E1, E4, E5, E6]. As the US Geological Survey (USGS) makes clear, ‘Neither the USGS nor any other scientists have ever predicted a major earthquake. We do not know how, and we do not expect to know how any time in the foreseeable future’ [E7]. In any case, what is needed is to lower the vulnerability of infrastructure and improve the accuracy of hazard assessment and the monitoring of faults, solutions proven in the USA, Japan and elsewhere. Faith in short-term forecasting endured partly because of a lack of local scientific expertise within developing nations. EwF has helped to address this within the framework of a supportive international partnership, through the empowerment of local scientists attached to 26 international partners across 11 different countries. The UNESCO Abdus Salam International Centre for Theoretical Physics describes how ‘EwF contributed effectively in fighting against the brain drain and isolation of scientists in developing countries’ [E5]. EwF is ‘clearly unique…it builds a tradition and legacy not like other initiatives which have hampered the development of in country science and discourage any growth of sustainable local research in the developing world’ [E5].
EwF also contributed to increasing ‘ the credibility and reputation of the EwF partnership members in their own countries’ [E5]. This has influenced the political mind-set, as described by the National Society of Earthquake Technology (NSET): ‘The presence of people from Italy, Nepal, China and Iran all saying the same things to politicians had more impact than in isolation’ [E2]. This has had an impact on public policy in terms of the development of building codes, the retrofitting of buildings, and the revision of city development planning, but it has also shifted the political focus of public safety policy away from short term prediction and towards increasing resilience. In Pakistan, for example, the National Disaster Management Agency has ‘started investing in preparedness and prevention rather than being just a post-disaster agency’ [E5].
Safer and more cost-effective hydrocarbon exploration
Hydrocarbon exploration in the Caspian Sea is high risk as a result of earthquakes and over-pressured sub-surface fluids, but attracts huge investments. These include more than USD 50 billion in the Kashagan field [E8], and a USD 6 billion BP project with Azerbaijan [E9]. The Arup Geohazard and Risk Management Team delivers natural hazard and risk assessment projects for clients worldwide including The World Bank, BP, Shell, HSBC, and others. Jackson and colleagues have advised Arup on assessment of seismic hazard and risk to:
BP, for their offshore facilities in the Central Caspian region. As Arup have testified, the ‘alignments of mapped geological faults and their characteristics were essential for the seismic hazard assessment’ [E10].
BP’s gas processing and export facility at Sangachal in Azerbaijan, one of the world's largest oil and gas terminals. Jackson was able to share recent research on the depth at which earthquakes occur in the region. This insight had a ‘ significant impact on the calculated earthquake ground shaking that would potentially occur at the surface and resulted in a safer and more cost-effective design for the oil and gas facilities’ [E10].
5. Sources to corroborate the impact
Earthquakes without Frontiers: Final Report. https://www.esc.cam.ac.uk/ewf/final-workshop-report-pdf See pg. 1 for population exposed to earthquake risk; pg. 2 for belief in prediction
Testimonial from National Society for Earthquake Technology (NSET) Nepal
Testimonial from Chief Scientific Advisor to HM Government
Testimonial from the Geological Survey of Iran. A ministry of the government of Iran and an EwF partner.
Testimonial from the International Center for Theoretical Physics (UNESCO). This UNESCO-run organisation is a partner in EwF and is committed to scientific education in developing countries.
**Testimonial from The Yessenov Foundation, Kazakhstan . A Kazakh charity committed to scientific education, and the principal sponsor of our major international conference in Almaty in 2016 in which they secured the participation of the mayor: http://yessenovfoundation.org/en/konferentsiya-po-zemletryaseniyam/.
USGS ‘Can you predict earthquakes?’ https://www.usgs.gov/faqs/can-you-predict-earthquakes?qt-news_science_products=0#qt-news_science_products
Media article ‘In a Prize for Big Oil Firms, Caspian Deal Eases Access’ New York Times, 8 October 2018. https://www.nytimes.com/2018/10/08/business/energy-environment/caspian-sea-deal-eases-access.html.
Media article, ‘BP seals new $6bn pact to drill for oil under the Caspian Sea’ The Telegraph, 19 April 2019. https://www.telegraph.co.uk/business/2019/04/19/bp-seals-new-6bn-pact-drill-oil-caspian-sea/.
E10 Testimonial Ove Arup & partners.
- Submitting institution
- University of Cambridge
- Unit of assessment
- 7 - Earth Systems and Environmental Sciences
- Summary impact type
- Technological
- Is this case study continued from a case study submitted in 2014?
- Yes
1. Summary of the impact
University of Cambridge researchers developed the first automated network of ultra-violet sensors to monitor volcanic gases at active volcanoes. Since the initial work on prototype instrumentation in 2002, the design has been implemented on 42 volcanoes across 18 countries and five continents. Sensors have been developed to be mounted on unmanned aerial vehicles, which allows monitoring of highly active and difficult-to-access volcanoes. Worldwide, 500 million people live in areas at risk from volcanic eruptions. The impact of this research has been to:
Protect life, property and livelihoods through:
enhancing the capability of volcano observatories worldwide to forecast eruptive activity in order to provide warning of imminent eruptions
providing critical input into government decisions leading to a) evacuations and b) mandatory exclusion zones
Allow safe industrial re-development (e.g. geothermal on Montserrat)
Allow the people of Manam to stay on their own land, rather than being permanently displaced, through developing the ABOVE project community-led resilience programme
2. Underpinning research
Up to the mid-2000s, volcanoes were monitored largely using the occurrence of earthquakes and displacements of the ground surface, because these data were available at a high temporal resolution (several measurements every second) and were a reliable indicator of magma movement. Geochemical monitoring, which yields the only direct indication of magma close to the surface, was in its infancy, yet increases in gas fluxes from volcanoes often preceded eruptions and so provided a tantalising yet untapped source of information about eruptive activity. Gas flux data were available so infrequently (once per day or per week, using cumbersome instrumentation) that their utility was severely limited, despite their potential to track magma ascent and forecast eruption style.
Sulfur dioxide (SO2) fluxes are a critical part of volcano monitoring. When magma ascends towards the surface and decompresses, sulphur exsolves from silicate melt and enters the gas phase. This process is analogous to removing the cork from champagne, which results in CO2 bubbles forming. The gas phase may migrate to the surface ahead of the magma, through permeable bubble networks. Increases in gas flux (SO2 is one of the primary gas species, the others are H2O and CO2) therefore indicate the impending arrival of magma to the surface, i.e. they can be used, in tandem with seismicity and ground displacements, to forecast eruptions [R1].
The impact described in this case was underpinned by research that took place within the Department of Earth Sciences at the University of Cambridge between 2002-2019, during which time a miniaturised UV spectrometer was developed for measurement of volcanic sulphur dioxide [R2] and the first network of scanning UV spectrometers was installed at volcanoes by Edmonds, Oppenheimer and co-workers [R3, 4]. A network of three UV spectrometers was developed and installed in Montserrat during the eruption of the Soufriere Hills Volcano in 2002 [R2, 3], whereby the spectrometers were connected to a scanning optical assembly and fibre optic cable, with power and telemetry, and code – which was made widely available - was written to both acquire spectra and to retrieve SO2 column amounts. SO2 column amounts were combined with meteorological data to derive SO2 fluxes every few minutes through the day, allowing the geochemical and geophysical data to be compared and interpreted on similar timescales, revolutionising the integrated monitoring of volcanoes [R1, R5].
This development provided the model and basis for UV spectrometer networks elsewhere [e.g. R3]. In 2006, a modification of the instrument was awarded a US patent (number 7,148,488: "Apparatus for measuring radiation and method of use"); Oppenheimer is a co-holder of the patent and the instrument described has been distributed under the name of ‘FLYSPEC’. Scanning spectrometer networks were installed on 42 volcanoes (for context, around 50-60 volcanoes erupt every year) across five continents between 2002 and 2020 ( 27 since 2013, the period covered by this impact case) by a number of research groups (e.g. EU-funded NOVAC, led by PI B. Galle, Chalmers University, co-I Oppenheimer) and volcano observatories , based on the design of the first installation in Montserrat, West Indies in 2002.
The advent of unmanned aerial vehicle (UAV) technology provided the opportunity for the ABOVE project, led by University of Cambridge researchers Liu and Edmonds, funded by the Alfred P Sloan Foundation, and including collaborators from the University of Bristol, USA, New Zealand, Germany, Sweden, Papua New Guinea and Costa Rica. The project developed cheap and portable sensors that could be mounted on UAVs to be flown into dangerous, highly active and difficult-to-access volcanoes [R6]. The data from these sensors showed previously unrecognised patterns in gas emissions related to bubble bursting, puffing and conduit dynamics [R6]. Subsequently, field campaigns to Guatemala, Montserrat and Papua New Guinea (places with active volcanoes and particularly vulnerable populations) in 2017-2019 have established these UAV-based methods, through training and sharing knowledge, as part of the regular toolkit of local volcano observatories for monitoring and hazard assessment.
Following the eruption of the White Island volcano in New Zealand in December 2019, and the tragic loss of life that followed, Edmonds was asked in August 2020 to provide consultant expert advice on gas monitoring data to the New Zealand Health and Safety Executive (Worksafe).
3. References to the research
The following peer-reviewed papers were all published in broad, high impact Earth Science journals, and are of a quality that is excellent/world-leading in terms of originality, significance and rigour.
2010 Christopher T, Edmonds M, Humphreys M, Herd RA. Volcanic gas emissions from Soufrière Hills Volcano, Montserrat 1995–2009, with implications for mafic magma supply and degassing. Geophysical Research Letters. 2010 Oct 1;37(19). https://doi.org/10.1029/2009GL041325
2003 Galle B, Oppenheimer C, Geyer A, McGonigle AJ, Edmonds M, Horrocks L. A miniaturised ultraviolet spectrometer for remote sensing of SO2 fluxes: a new tool for volcano surveillance. Journal of Volcanology and Geothermal Research. 119(1-4):241-54. https://doi.org/10.1016/S0377-0273(02)00356-6
2003 Edmonds M, Herd RA, Galle B, Oppenheimer CM. Automated, high time-resolution measurements of SO2 flux at Soufrière Hills Volcano, Montserrat. Bulletin of Volcanology. 65(8):578-86. https://doi.org/10.1007/s00445-003-0286-x
2003 McGonigle AJ, Oppenheimer C, Hayes AR, Galle B, Edmonds M, Caltabiano T, Salerno G, Burton M, Mather TA. Sulphur dioxide fluxes from Mount Etna, Vulcano, and Stromboli measured with an automated scanning ultraviolet spectrometer. Journal of Geophysical Research: Solid Earth. 108(B9). https://doi.org/10.1029/2002JB002261
2008 Rodríguez LA, Watson IM, Edmonds M, Ryan G, Hards V, Oppenheimer CM, Bluth GJ. SO2 loss rates in the plume emitted by Soufrière Hills volcano, Montserrat. Journal of Volcanology and Geothermal Research. 2008 Jun 1;173(1-2):135-47. https://doi.org/10.1016/j.jvolgeores.2008.01.003
2019 Liu EJ, Wood K, Mason E, Edmonds M, Aiuppa A, Giudice G, Bitetto M, Francofonte V, Burrow S, Richardson T, Watson M. Dynamics of outgassing and plume transport revealed by proximal Unmanned Aerial System (UAS) measurements at Volcán Villarrica, Chile. Geochemistry, Geophysics, Geosystems. 20(2):730-50. http://dx.doi.org/10.1029/2018GC007692
Grants:
2007: PI Edmonds, Royal Society Grant – installation of gas sensors, GBP15,000
2010: PI Edmonds, Deep Carbon Observatory DECADE grant for development of gas sensors, USD15,000
2014-2017: Co-I Edmonds, Centre for the Observation and Modeling of Earthquakes and Tectonics (NERC, COMET) GBP1.2M total, GBP153,757 to Cambridge
2018-2019: PI Liu, Co-I Edmonds, Alfred P Sloan Foundation GBP180,000, ‘ABOVE’: to use sensors mounted on unmanned aerial vehicles to quantify volcanic gas emissions from Papua New Guinea.
2005-2010: participant Oppenheimer (PI Galle, Chalmers University), FP6: Network for Observation of Volcanic and Atmospheric Change (NOVAC), GBP112,280.
4. Details of the impact
Worldwide, 500 million people live in areas at risk from volcanic eruptions [E1]. The spectrometer networks first developed by Edmonds and colleagues at the University of Cambridge have been adopted by volcanological observatories on 42 volcanoes (27 since 2013) across 18 countries and five continents [E2, E3]. They are used to protect life, property and livelihoods through forecasting eruptive activity and informing critical decisions on evacuations and exclusion zones; to allow safe industrial re-development; and – through the ABOVE project resilience programme (Aerial-Based Observations of Volcanic Emissions) - to allow the Manam islanders to remain on their island.
Forecasting Eruptive Activity and providing warning of imminent eruptions
The Institute of Geological & Nuclear Sciences (GNS), New Zealand, were among the first government bodies to develop a spectrometer system based on the design Edmonds and colleagues pioneered. Senior Scientist at GNS, Dr Craig Miller, states [E4]:
‘the UV scanning spectrometer network installed by Edmonds, Oppenheimer and colleagues in Montserrat provided the template for GNS volcanologists to develop a similar system at White Island, New Zealand. It is used for monitoring volcanic activity at this hazardous and unpredictable volcano. An increase in gas flux, along with increased levels of seismicity and ground deformation, would significantly increase the probability of eruption and consequently the alert level at the volcano, which is used for decision-making surrounding issues such as restricting access and warnings to the public’.
In October 2019, SO2 fluxes measured by the scanning spectrometers (and accompanying tremor) at White Island increased to the highest levels since 2016, suggesting an eruption was imminent over the coming weeks and months [E5, 6]. On 18 November 2019, the alert level was raised to ‘2’ (the highest before eruption) signalling ‘heightened volcanic unrest’ and ‘potential for eruption hazards’ [E7].
Tragically, an eruption on 9 December 2019 killed 19 people. In this case, clear warnings were not heeded, and preventative action which could have saved lives was not taken.
At Volcán Tungurahua (Ecuador), 30,000 people live in areas at risk from pyroclastic flows and lahars. A spectrometer system based on the Cambridge design was installed in 2004. Eruptions in 2013, 2014 and 2016 have had considerable impacts on livelihoods, particularly agricultural activities (with crops damaged and land made unusable due to the deposition of volcanic ash). The scanning spectrometer stations provide SO2 flux data for the assessment of risk and early warning of eruptions. In February 2014 >600 people were evacuated after alert levels were raised in response to increasing SO2 flux (to over 2000 tonnes per day), as well as increased rates of earthquakes and ash venting at the summit:
‘The automatic scanning DOAS stations as first developed at Soufriere Hills
Volcano, and which nice results have been shown by Edmonds and colleagues in 2003,
have been widely adopted by volcanological observatories over the past 15 years… At Tungurahua, we installed 2 DOAS systems directly based on the Montserrat UV
spectrometer system, the UV scanning spectrometer network yielded important data which,
when used in combination with other monitored parameters as seismic activity, allowed us
to assess hazard levels and advise local authorities on the general level of volcanic
activity’ [E3, Instituto Geofisico, Ecuador] .
Providing critical input into mandatory exclusion zones
In Montserrat, the eruption of the Soufriere Hills Volcano ceased in 2011, yet it remains restless. One key characteristic is continued high flux of SO2, as measured by the spectrometer network, leading the government to retain an exclusion zone around the volcano. The Montserrat Volcano Observatory (MVO) and Scientific Advisory Committee (British Foreign Office) continue to rely on the SO2 flux data to assess whether the eruption is over or has merely paused. The March 2019 MVO Scientific Report [E8] states:
‘the potential for continuing activity has been considered against the following three criteria:
Seismicity
Gas – daily SO2 emission rates above 50 tonnes per day
Ground deformation
Criteria 2 and 3 are currently being met.’
Consequently, the volcano remains in an elevated state of unrest, with an exclusion zone including over half the island.
Allowing safe industrial re-development
However, on Montserrat, the monitoring networks are now making economic recovery possible. The Government has permitted a geothermal plant to be established in the exclusion zone, a decision informed by advice from the MVO, based partly on gas flux information. The Director of the MVO [E9] states:
‘In 2014 the Government of Montserrat gave permission for a geothermal company, the Iceland Drilling Company , to begin operations generating two boreholes from which it was projected that much of the island’s energy needs would be provided. A third well is planned for 2020. This permission was based on advice from the Montserrat Volcano Observatory on volcanic risk; gas fluxes were one part of the critical evidence upon which the low risk level for that particular area was assigned.’
Test results indicate that geothermal power could generate more electricity than is needed by the island, freeing it from reliance on diesel-powered generators – among the most expensive electricity in the world – and reducing CO2 emissions by replacing fossil fuel generated electricity [E10].
Allowing islanders to remain on their land
The ABOVE project, led by University of Cambridge researchers Liu and Edmonds, involves field campaigns to Papua New Guinea volcanoes Rabaul and Manam to deploy UAV gas sensors and train local people in these techniques. Manam is a small island with > 2000 people, who are regularly evacuated to the mainland during eruptions every few years (there have been nine since 2000). Islanders live with extreme volcanic risk, as permanent relocation is unacceptable because the island is essential to their way of life and rehoming on the mainland brings risk of conflict. The UAV technology and training provided by the ABOVE project offers a means for them to remain. An ABOVE project video includes interviews with local people:
‘Those major eruptions [in 2004] were never addressed properly by the government… we have been waiting for 15 years and nothing is happening… We are regarded as IDPs – Internally Displaced Persons - on our own land.’[E11].
The ABOVE project provides equipment and training to the local volcano observatory to continue measurements of gas fluxes using UAVs. One representative from each province in Papua New Guinea came to the training workshop in February 2019 and, thereafter, successfully lobbied provincial governments for additional funding [E1]. The islanders had relied on visual monitoring, but now fly UAVs over the volcano to monitor gas flux and activity to see what and who is most at risk, allowing them to remain on their own land.
5. Sources to corroborate the impact
‘Above and Beyond’: the story of the ABOVE project https://www.cam.ac.uk/stories/activevolcano
Excerpt from NOVAC web page, showing the number of volcanoes with UV scanning spectrometers installed https://novac-community.org/volcanoes
Testimonial from Instituto Geofisico, Ecuador
Testimonial from Senior Scientist, Natural Hazards Division, GNS Science, New Zealand
New Zealand news article describing elevated unrest at White Island, New Zealand, in October 2019, with details of high SO2 fluxes.
A second Zealand news article describing elevated unrest at White Island, New Zealand, in October 2019, with details of high SO2 fluxes.
Geonet, Volcanic Alert Bulletin, 18 November 2019. Geonet is the Volcano Monitoring Arm of GNS Science, the principal geological Government Agency in New Zealand.
MVO Scientific Report for Volcanic Activity between 1 October 2018 and 31 March 2019, Open File Report OFR 19-01, 7 June 2019. Montserrat Volcano Observatory. See page 37.
Testimonial from the Director of the Montserrat Volcano Observatory
The Iceland Drilling Company https://www.jardboranir.is/drilling-project-starting-in-montserrat/
The ABOVE project page https://deepcarbon.net/project/above#Overview