Introduction to this website

This website has, as its chief theme, the study of natural hazards.

As a senior lecturer in physical geography and natural hazards at Coventry University, my chief area of research (when not teaching) is using remote sensing techniques to monitor natural hazard phenomena (mainly volcanoes and earthquakes). Key natural hazards occurring globally will be automatically posted daily (via RSS feed from NASA’s Earth Observatory).

I hope you find the material herein useful and interesting. If you have any comments then please contact me.

Unfortunately, I can only make the teaching section open to relevant students. You’re only missing lecture material and reading lists but if you’re really interested, why not come and take a Geography degree at Coventry Uni!?

Scoping visit to Central America

Matthew Blackett recently visited Guatemala, El Salvador and Nicaragua on university business. The trip had a number of objectives:

– to investigate possible student internship/work placements in these countries

– to assess the feasibility of conducting student fieldtrips within the region

– to meet with relevant parties to discuss research work under the themes of the Centre for Disaster Management and Hazards Research


In Guatemala we met with Dr Guerro of the ICC (Instituto Privado de Investigación sobre Cambio Climático / Private Institute for Climate Change Research) and the Executive Secretary of CONRED (Coordinadora Nacional para la Reducción de Desastres / Guatemala Disaster Civil Protection). We were fortunate to witness Fuego Volcano erupt (see below):

Fuego1 Fuego2

In El Salvador we met with FUNDASAL (Fundación Salvadoreña de Desarrollo y Vivienda Mínima), and were given a tour of their great work in the region. They work on improving the living standards of people either due to poverty or following disasters. We also met with the Heads of the British Embassy in San Salvador (see below), with researchers from the University of Central America and the University of El Salvador, with El Salvador’s Civil Protection body and with an NGO, Progressio, involved in arranging student trips to El Salvador.

San Sal

In Nicaragua, a tight schedule meant that arranged meeting with the NGO: Bona Fide and with the Instituto de Geología y Geofísica de Nicaragua IGG/CIGEO could not go ahead. However, a student placement is being arranged with the former and formal research discussions are continuing with the latter. We also had the opportunity to visit the active Masaya Volcano – a site with much potential for student fieldtrips:


Poor quality of some studies, alas

I do sometimes have concern over the whole peer review process whereby unfounded observations are claimed to exist. I’ve just found one example of this in the journal: Journal of the International Society for the Prevention and Mitigation of Natural Hazards. The article: “Geomorphological characteristics identification [sic.] from remote sensing along with surface temperature anomaly and SAR interferometry – related studies and their correlation with earthquake occurrences in Gujarat”, by Majumdar (2003) provides an examination of remotely sensed data which examines changes in both geomorphology and land surface temperature as associated with seismic activity in the Gujarat region of India. I don’t claim to be a geomorphological-seismological expert so I will leave that aspect be, but I do know something about thermal anomalies potentially preceding earthquakes – unfortunately the author of this paper seems not to.


What is presented are land surface temperature images (derived from NOAA TIR data) for the 3rd, 6th and 7th April 2006. An earthquake occurred in the region on 6th April. It is asserted that there was a sharp increase in land surface temperatures 3-6 April which subsequently fell on 7 April. I will agree, the images do appear to show something of this nature but … given just one year’s worth of data, how do we know whether or not this is a regular occurrence? Perhaps this increase in temperature occurs every year around 3-6 April. Perhaps this period displayed particularly clear skies, meaning that the land surface was warmer. Indeed, there could be any number of reasons for such an increase in temperature, many of which are not associated with the earthquake – none of these possibilities however, are examined or even acknowledged, in the paper. The least that is required is that comparison is made to other (non-earthquake) years to ensure that this is not a regular occurrence. Reference to climatic and meteorological data too, would confirm that the observation is not the result of these sorts of factors. I’m also a little bemused that my work was not cited anywhere in the work, but hey, perhaps I’ve not circulated it adequately.

There seems to be a lot of good research which doesn’t get published for various reasons, but also lots of poor work that does. Reviewers please do a thorough job – think through all possibilities and ways that a paper, and its findings, might be made stronger. This is for the betterment of science in general.

Visit to China University of Mining and Technology, Xuzhou, China

I was awarded funding from the Universities China Committee in London to visit Dr Qin Kai for research collaboration discussions. The visit went ahead over March and April 2014 and during the visit, I presented on my research into the monitoring of natural hazards via remote sensing. We were also able to discuss many potential research collaborations for the future, including with Professor Lixin Wu.



The official link from the university in China can be found here.

The first Landsat-8 thermal imagery of volcanic activity

Abstract of recently published paper

The Landsat-8 satellite of the Landsat Data Continuity Mission was launched by the National Aeronautics and Space Administration (NASA) in April 2013. Just weeks after it entered active service, its sensors observed activity at Paluweh Volcano, Indonesia.


Given that the image acquired was in the daytime, its shortwave infrared observations were contaminated with reflected solar radiation; however, those of the satellite’s Thermal Infrared Sensor (TIRS) show thermal emission from the volcano’s summit and flanks. These emissions detected in sensor’s band 10 (10.60–11.19 μm) have here been quantified in terms of radiant power, to confirm reports of the actual volcanic processes operating at the time of image acquisition, and to form an initial assessment of the TIRS in its volcanic observation capabilities. Data from band 11 have been neglected as its data have been shown to be unreliable at the time of writing. At the instant of image acquisition, the thermal emission of the volcano was found to be 345 MW. This value is shown to be on the same order of magnitude as similarly timed NASA Earth Observing System (EOS) Moderate Resolution Imaging Spectroradiometer thermal observations. Given its unique characteristics, the TIRS shows much potential for providing useful, detailed and accurate volcanic observations in the future.

Available at:

Earthquakes changing the character of the ionosphere?

Review of: He, L.M., Wu, L.X., De Santis, A., Liu, S.J. and Yang, Y. (2014). Is there a one-to-one correspondence between ionsopheric anomalies and large earthquakes along Longmenshan faults? Annales Geophysicae (accepted).

This is a very interesting and timely paper. Interesting as it both shows evidence of one potential precursor to a particular earthquake (Wenchuan, China, May 2008) and, in relation to another earthquake event, shows evidence against the presence of such precursors (Ya’an, China, April 2013). This suggests the paper will be completely balanced. The paper is timely as, despite having been around for a long time, wavelets are now increasingly being used to quantify geophysical phenomena that provide a non-stationary signal (one case in point: Murphy et al. 2013, concerning periodic episodes of thermal emissions from various volcanoes).

The authors propose precursors which relate to phenomena in the ionosphere. This part of the atmosphere is influenced by many factors including solar and geomagnetic phenomena and as such, these ‘normal’ signals need to be removed from those which might be pre-seismic and to do this, a method of removing the background signal is presented (first discussed in He et al. 2012). The dataset analysed is from the global navigation satellite system and consists of the total electron content (TEC) of the ionosphere, which reflects irregularities of the ionosphere. The TEC signal was initially smoothed, so as to remove diurnal and seasonal patterns. Two wavelet methods were then applied to the dataset: the analytic wavelet transform (AWT), to detect variability in the TEC, and the cross-wavelet transform (XWT), to determine whether the changes were associated with the impending earthquake. The XWT is most pertinent here as it is applied to determine any ‘mutual relationship of two time series in the time-frequency domain’ (pg. 8); these two timeseries here are the ionospheric signal and any geophysical indices.

In relation to the Wenchuan earthquake, the solar activity was found to be low and as such, did not pollute any potentially seismic signals. What was found were signals over the region of the subsequent earthquake that were unusual, not happening in previous years or anywhere else at the same latitude; indeed they appear to be over the location of the impending earthquake (see below).


In relation the Ya’an earthquake however, the period was associated with high solar activity which had to be removed from the signal. Even applying these methods, no ionospheric anomalies could be found in the month prior to the earthquake. Interestingly, the authors note that had they not applied their own method of noise removal, they might well have concluded that these large signals were associated with the impending earthquake.

So evidently, the authors acknowledge that they do not know everything about these observations and that they cannot predict earthquakes on their basis, but what they have shown is a line of enquiry which should be explored more thoroughly. What you may be wondering however, is: how can an earthquake possibly cause changes in the ionosphere? Well the theory postulated is that radon emanations appear to increase prior to an earthquake (this is a widely proven observations see e.g. Choubey et al. 2004). This gas could ionise the lower atmosphere and as such, affect the electrical characteristics of the entire atmospheric column. Electromagnetic energy generated on rock compression (noted in Ouzounov and Freund, 2004) is also claimed as having a potential influence. So why then do some earthquakes seemingly produce such effects and other don’t? Well it might all be down to the size of the forthcoming earthquake (a greater magnitude earthquake releasing more energy), or the formation of the lithosphere which could potentially augment, or shield, some of the effects from the atmosphere.

Overall, this is an interesting study and it is great to see the presentation of both positive and negative results.  I guess like most things in this field, more data is required to prove, categorically, the presence (or otherwise) of such phenomena. This work is a good step in that direction. In terms of methods applied too, this work could potentially form a reference piece for the application of wavelets. It explains their function much more comprehensively than most other studies do and, given that large proportions of scientific research focus on attempting to find correlations between datasets, the presentation of the methods that can be applied to do that  is very useful. Let’s hope more research continues in the field, using techniques such as these, to confirm or refute the presence of earthquake precursors convincingly and/or, like this paper, to explain apparent anomalies.


Choubey, V.M., Mukherjee, P.K. and Ramola, R.C. (2004). Radon variation in spring water before and after Chamoli earthquake, Garhwal Himalaya, India. In: Proceeding of 11th International Congress of the International Radiation Protection Association. Madrid, Spain, 23-28 May.

He, L., Wu, L., Pulinets, S., Liu, S. and Yang, F. (2012). A nonlinear background removal method for seismo-ionospheric anomaly analysis under a complex solar activity scenario: A case study of the M9.0 Tohoku earthquake. Advances in Space Research, 50, 211–220.

Murphy, S.W., Wright, R., Oppenheimer, C. and Souza Filho, C.R., 2013, MODIS and ASTER synergy for characterizing thermal volcanic activity, Remote Sensing of Environment, 131, 195–205.

Ouzounov, D. and Freund, F. (2004). Mid-infrared emission prior to strong earthquakes analyzed by remote sensing data. Adv Space Res, 33, 268–273.