Showing posts with label SE. Asia. Show all posts
Showing posts with label SE. Asia. Show all posts

Tuesday, May 26, 2009

Landslides from Cyclone Alia in Darjeeling

One of the most admirable landslide websites that I know is the Save the Hills blog, which is the mouthpiece of a community level group trying to raise awareness of the problems of landslides in Darjeeling in NE India. I have featured this site several times before.

As Cyclone Alia has closed in on the area over the last few days See below) they have been warning of the danger of landslides triggered by the rainfall that the cyclone would inevitably bring. The Cyclone passed across the area yesterday - and sure enough reports are now emerging of the landslides that the rainfall has triggered. At the time of writing Sify is reporting 22 killed in landslides, with 10 injured and another six people reported missing. Over 100 landslides have been reported. The Times of India reports that 245 mm of rainfall fell in a 24 hour period.

Meanwhile, in the last few days there are also reports of a large landslide in Sialum District in Morobe province of Papua New Guinea, which is reported to have killed 19 people (although the picture is still rather unclear), landslides in Bhutan with at least one fatality, mudslides in Uttar Pradesh in India that killed eight people, and landslides in Guangdong that have killed four. Finally, there are some very unclear reports about the magnitude of the impact of heavy rainfall in Afghanistan, with reports of about 95 people killed in landslides and floods.

Sadly, none of this is particularly unusual as we are seeing the impacts of the development of the summer monsoon across Asia.

Thursday, March 12, 2009

Climate Change Vulnerability Mapping for Southeast Asia

A very interesting report was released last week by the Economy and Environment Program for Southeast Asia (EEPSEA) in which an attempt has been made to map the pattern of vulnerability across the region to climate change. The aim of the project, for which the report is available online, was to "identify which regions in Southeast Asia are the most vulnerable to climate change." This is a fairly bold thing to try to do, so lets take a look at what they have achieved and how they have done so.

The researchers have taken as a starting point maps of five hazards - cyclones, drought, floods, landslides and coastal inundation (sea level change). In each case they have used an external dataset to indicate the hazard associated with each of these events - so, for example, for landslides they have used the NGI landslide hazard maps produced in the World Bank Natural Disaster Hotspots project (Fig. 1), whereas for sea level change they have modelled the inundation associated with a 5 m increase in sea level.

Fig 1: NGI landslide hazard map used as an input into the Climate Change Vulnerability Map.

For each hazard a scale of 1-10 has been used, with 10 being highest hazard and 1 the lowest. For each cell on the map, the average score across the five hazards was then taken as an indication of the overall hazard. I will return to this below. The outcome of this analysis is termed the "Multiple Climate Hazard Index". The resultant map is shown in Fig. 2 below.

Fig 2: The Multiple Climate Hazard Map.

This map has then been combined with data for population density (incorporating areas that are ecologically protected) and "adaptive capability" (defined as "the degree to which adjustments in practices, processes, or structures can moderate or offset potential damage or take advantage of opportunities (from climate change)." The latter has used expert judgement to create an index based upon data on education, poverty, income inequality and suchlike. These three indicators have then been averaged to determine the level of vulnerability to climate change (Fig. 3).

Fig 3: The Climate Change Vulnerability Map.

Hmmmm! First, let me say that this is a brave thing to do - such exercises are really challenging given the complexity of the dataset. Such exercises are important and useful given the need to prioritise. I am hesitant to be too critical. I would however like to point out four things that are worth thinking about.

1. Perhaps most importantly, I don't see how this is a map of climate change vulnerability. An argument can be made that this is a map of vulnerability to meteorologically driven hazards, but most of the parameters do not appear to consider a changing climate. The data for floods, droughts and cyclones used historic data of occurrence. This does not consider change. The only parameter that considered climate change was the sea level inundation, but this used a terribly simplistic model (a binary switch at 5 m sea level rise).
2. The decision to average across the five hazards is strange. The problem can be illustrated with an extreme example. Imagine you live on a flat, tropical plain 20 cm above sea level. Most of the hazards are likely to be low - no landslides, no river floods, no droughts, no tropical cyclones. However, a comparatively small rise in sea level wipes you out. In the system used here, your hazard comes out low whereas actually it is very high. It might be more rationale to take the highest value of hazard, or a more subtle measure.
3. The decision to weight the parameters equally is also interesting and surprising. Given the vastly different impact of the hazards, it might be worth weighting the hazards appropriately.
4. The decision to average the hazard, the population and adaptive capability is also odd. I would have thought that these parameters should be combined so that they interact (r.g. through multiplication and/or division). Clearly, the case where the level of hazard is high, the population is high and the adaptive capacity is low is exactly where really serious disasters occur.

I suspect that this map needs another iteration or two, perhaps backed up with a sensitivity analysis, but as a first step the authors deserve praise.

Monday, November 3, 2008

Malaysia talk

The following is my presentation at the International Symposium on Slopes in Kuala Lumpur, Malaysia. It is an invited paper on the topic of landslides in Asia in relation to climate change and other environmental pressures. I hope you find it of interest.

The file should appear below:


Uploaded on authorSTREAM by Dr_Dave

If you cannot see the file then click on the highlighted Dr_Dave link above. The full Powerpoint file can be downloaded from that location too. I will post a report on the most interesting parts of Day One tomorrow.

Wednesday, August 27, 2008

The influence of the summer monsoon on fatal landslides in Asia

I am currently putting together a keynote paper for the forthcoming International Conference on Slopes, which is being held in Malaysia in November. I have been looking at the occurrence of fatal landslides in Asia, using the Durham Landslide Database as the source of data. I have plotted the number of fatal landslides by month for 2002-2007 for three areas - South Asia (i.e. the Indian subcontinent), East Asia (which includes China, Taiwan, Korea and Japan) and SE. Asia (which should be self evident). The graphs are shown below (note the different magnitudes of the y-axis scales by the way).

First, South Asia shows a very strong monsoon signal. Look in particular at the mean trend for the five years. The level of fatal landsliding in the winter months is very low, with most of the events occurring in June to September. It is also clear that the number of landslides increases rapidly at the start of the monsoon as the rain bands push northwards, but then decline slowly as the monsoon disperses. There is also considerable year-on-year variation; in particular the very strong and prolonged monsoon rainfall across parts of India is very clear for 2007.

East Asia (below) also shows a strong monsoon signal, of course slightly modified by the impact of typhoons too. Here though the pattern is quite different - again look at the graph of the mean of the other data. In this case the monsoon signal is far more symmetrical, again reaching a peak in July but rising and declining at about the same rate. Again there is considerable year-one-year variation both in terms of number of events and the variation through the year. The big spike in July 2006 is particularly clear.

SE. Asia present a completely different picture (below). As much of SE. Asia is tropical there is far less monthly variation. Unsurprisingly no monsoon spike is seen. The occurrence of landslides is slightly higher in the latter part of the year as the rainy season affects Indonesia for example. Of particular note are the variations in the distribution between years - this really does reflect the occurrence of extreme tropical cloud bursts.


So the impact of the really large scale climate systems on Asian landslides is absolutely clear. This is particularly interesting in the context of climate change - exactly how the Asian monsoon in particular will change will partially determine the landslide impact. Unfortunately the models are not resolving this issue too well at the moment, but most do suggest an increase in the occurrence of the most intense rainfall events. The implications for landslides of this are stark.

Friday, April 25, 2008

Updated: 25th April: The Kaiapit Landslide, Papua New Guinea, 1988

Update: Mark Drechsler has provided some images of the Kaiapit landslide, which are now integrated into the text below. Thanks to Mark for this - it is much appreciated. All images copyright of Mark Drechsler. In addition, I have placed a copy of the Drechsler et al (1989) paper on the International Landslide Centre website here. It provides a fascinating level of detail about the slide. I recommend this paper over and above the alternative.


Click on the images for a full-sized view - it is well worth it!

Original text: Thanks for Mark Drechsler of Parsons Brinkerhoff Australia and the University of Adelaide for reminding me of the Kaiapit Landslide, which is surely one of the largest landslides of the last two decades (can anyone think of any larger?). Even though its impact was not enormous (74 deaths in three villages) the scale of this landslide is staggering. The landslide was described in a paper by Dreschler et al. (1989) and one by Peart (1991), from which these details are taken.

The slope failed at 10:43 am on 6th September 1988 when approximately 1.8 cubic kilometres of mountian collapsed, leaving a scar 1600 m high. The debris ran out over a distance of 6.5 km, covering an area of over 11 square kilometres. The estimated velocity is up to 180 km/hour. The slide inundated three villages and formed four valley-blockage lakes.

What is particularly interesting about this slide is the lack of an obvious trigger. Peart (1991) reported that the time of initiation was not the rainy season (indeed it was towards the end of the dry season) and that the period in question was not particularly wet. No seismic activity was recorded. The area has not been glaciated, so over-steepening and loss of support cannot be a cause. Clearly the area is affected by high levels of uplift, which may have allowed the formation of over-steepened slopes. These are probably a causal factor, but do not explain the triggering.

Peart (1991) sagely suggested that there may have been a time-related factor in the initiation of the landslide. I am convinced that time-dependent behaviour is important for large-scale landslide triggering, which means that the time of failure might lag significantly behind the trigger event. This is not always the case, but quite often very large landslides do not have an obvious trigger event. Other examples include the Mount Cook failure in New Zealand and the Leyte landslide in the Philippines.

Sadly the Google Earth imagery of the slide site is covered by clouds. Comments are welcome as ever.

Reference
Drechsler, M. Ripper, I., Rooke, E. and Warren, E. 1989. The Kaiapit Landslide, Papua New Guinea. In: Engineering Geology in Tropical Terrains, Universiti Kebaangsan Malaysia.
Peart, M. 1991. The Kaiapit landslide: events and mechanisms. Quarterly Journal of Engineering Geology, 24, 399-411.


Hat-tip: Mark Drechsler from Parsons Brinckerhoff and University of Adelaide.

Sunday, December 16, 2007

Vietnam landslide

There are newswire reports of a nasty landslide in central Vietnam. The reports suggest that this was a rockslide in the morning of 15th December in Tuong Duong district of central Nghe An province triggered by quarrying as part of a hydroelectric powerplant scheme. The number of workers buried is 18. Looking at the picture available here there is little chance of any survivors. The unfortunate victims appear to all have been workers on the powerplant.

Reports on 16th December suggest that the landslide had a volume of about 500,000 cubic metres, burying the victims to a depth of between 30 and 50 m. It is unsurprising then that only three bodies have been recovered to date.

Update (18th December): Thanh Nien reports that eight bodies have now been recovered, but that the rescue operations are proving to be difficult and hazardous. No clear cause of the collapse is evident but "Workers speculated Saturday that an explosion carried out on Friday might have weakened the mountain's structure and caused the landslide, but their theory has yet to be verified or disproved". Certainly poorly planned and/or executed blasting can be the cause of collapses, so it will be interesting to hear whether this is the case here.