Climate History Controls Future Landslide Hazard
Lead Research Organisation:
Cardiff University
Abstract
The intense precipitation associated with large storms can initiate thousands of landslides and debris flows, endangering lives and cause significant damage to infrastructure. Changes to the frequency and/or intensity of storms is a predicted consequence of anthropogenically-driven climate change (Rosenzweig et al., 2007), thus predictive models of landsliding are essential for mitigating these effects. Shallow landslides that initiate in soil are particularly destructive as they often initiate rapidly moving debris flows. Physically-based shallow landslide hazard models usually estimate landsliding a function of modern hydrologic, ecologic, and soil mechanical properties (Montgomery and Dietrich, 1994; Pack et al., 2001). The flaw in this approach is that it does not account for the "memory" of previous landslides in a catchment, where landslides are unlikely to occur twice in the same location within the short window of time (<1000 years). When landslide "memory" is considered, we hypothesise two possible effects on future landsliding: (1) the likelihood that extreme rainfall will create a large landslide event is dependent on the number of large storms that have recently occurred in a catchment, and (2) storms that initiate a 1000's of landslides may have a resonance within a landscape that causes landslides to cluster in time. Accounting for the combined role of precipitation and landscape resonance is of immediate concern as we begin to make predict hazards associated with climate change. The proposed research will quantify whether landslides are clustered in time, through the collection of a novel, large, millennial-scale dataset of landslide frequency. We will analyse landslide frequency using radiocarbon found at the base of 75 hollows (local depocentres located 10's of metres above channel heads) where shallow landslides initiate. These data, in conjunction with high resolution LiDAR topographic data, will drive the creation of a unique, probabilistic, landslide hazard model that estimates landslide hazard based on both recent precipitation and the potential resonance imparted by previous storms. Our novel landslide dataset and landslide hazard model will significantly improve our ability to predict the risks posed by landslides in current and future climate scenarios.
Planned Impact
Who will benefit from this research?
This proposal models the debris flow hazard potential as a function of climate. Debris flows are a global hazard, affecting soil-mantled landscapes of high relief and precipitation. The primary beneficiaries of this exercise are the disaster management industry (particularly the insurance industry) and policy-makers from local and regional governments. Facilitating informed decision-making is therefore the key focus of our impact plan. We have identified two key groups that will benefit: (1) Our specific focus on North Carolina will benefit the policy-makers and insurance in this area, particularly as they make decision regarding proposed steep slope legislation. (2) The probabilistic basis of our model can be applied to any mountain range that is affected by debris flows, making this study of general interest to companies and policy-makers in debris flow-prone regions (e.g. Scottish regional governments, Swiss government).
How will they benefit from this research?
The key benefit from this research for both governmental and industrial partners is the ability to make decisions that are better informed by data. The advance provided by the modelling approach enables users of the model to explore how debris flow potential varies with different climate scenarios. Governmental organisations will be able to make informed decisions about the type of zoning and landuse restrictions that can occur in mountainous catchments. The insurance industry can use the model output to decide how best to insure infrastructure and property in areas prone to debris flows. The uniqueness of the model means that while it is of use within a British context, it can be exported to other countries and to Bristish industries working in these countries.
This proposal models the debris flow hazard potential as a function of climate. Debris flows are a global hazard, affecting soil-mantled landscapes of high relief and precipitation. The primary beneficiaries of this exercise are the disaster management industry (particularly the insurance industry) and policy-makers from local and regional governments. Facilitating informed decision-making is therefore the key focus of our impact plan. We have identified two key groups that will benefit: (1) Our specific focus on North Carolina will benefit the policy-makers and insurance in this area, particularly as they make decision regarding proposed steep slope legislation. (2) The probabilistic basis of our model can be applied to any mountain range that is affected by debris flows, making this study of general interest to companies and policy-makers in debris flow-prone regions (e.g. Scottish regional governments, Swiss government).
How will they benefit from this research?
The key benefit from this research for both governmental and industrial partners is the ability to make decisions that are better informed by data. The advance provided by the modelling approach enables users of the model to explore how debris flow potential varies with different climate scenarios. Governmental organisations will be able to make informed decisions about the type of zoning and landuse restrictions that can occur in mountainous catchments. The insurance industry can use the model output to decide how best to insure infrastructure and property in areas prone to debris flows. The uniqueness of the model means that while it is of use within a British context, it can be exported to other countries and to Bristish industries working in these countries.
People |
ORCID iD |
Tristram Hales (Principal Investigator) |
Publications

Clubb F
(2014)
Objective extraction of channel heads from high-resolution topographic data
in Water Resources Research

Grieve S
(2016)
How long is a hillslope? How long is a hillslope?
in Earth Surface Processes and Landforms

Grieve S
(2018)
Controls on Zero-Order Basin Morphology
in Journal of Geophysical Research: Earth Surface

Hales T
(2017)
Soil moisture causes dynamic adjustments to root reinforcement that reduce slope stability Dynamic slope stability due to roots
in Earth Surface Processes and Landforms

Mudd S
(2014)
A statistical framework to quantify spatial variation in channel gradients using the integral method of channel profile analysis CHANNEL SEGMENT FITTING
in Journal of Geophysical Research: Earth Surface

Parker R
(2017)
Spatial prediction of earthquake-induced landslide probability

Parker RN
(2016)
Colluvium supply in humid regions limits the frequency of storm-triggered landslides.
in Scientific reports
Description | We have been exploring the relationship between landslides and extreme weather events. Our initial results suggest that future landslide hazards are dependant on the history of land sliding in a particular area rather than future precipitation events. We are developing a model that will improve our ability to predict future landslide hazards by accounting for past landslide rates. We have also quantified how landslides vary with different precipitation frequencies |
Exploitation Route | Our model can be applied to any area of the planet that is susceptible to shallow landslide hazards. We are developing a web-based tool that can be used to predict possible landslide potential for landscapes |
Sectors | Education,Environment,Leisure Activities, including Sports, Recreation and Tourism |
Description | Increasing Resilience to Natural Hazards in China |
Amount | £500,000 (GBP) |
Organisation | Natural Environment Research Council |
Sector | Public |
Country | United Kingdom |
Start | 01/2016 |
End | 01/2019 |
Description | NERC Cosmogenic Isotope Facility Grant |
Amount | £23,600 (GBP) |
Funding ID | 9145/0414 |
Organisation | University of Glasgow |
Department | NERC SUERC CIAF Cosmogenic Isotope Analysis Facility |
Sector | Academic/University |
Country | United Kingdom |
Start | 07/2014 |
End | 12/2015 |
Description | Chengdu University of Technology Partnership |
Organisation | Chengdu University of Technology |
Department | State Key Laboratory of Geohazard Prevention and Geoenvironmental Protection |
Country | China |
Sector | Academic/University |
PI Contribution | We developed a secondary proposal submitted to the IRNHiC call to NERC/ESRC/NSFC/Newton Fund that was successful. This develops the work that we have done on rainfall induced landslides. |
Collaborator Contribution | The were collaborators on the proposal development and have provided access to facilities and equipment. |
Impact | The main output was the development of a successful research proposal. |
Start Year | 2015 |
Description | Coweeta |
Organisation | U.S. Department of Agriculture USDA |
Department | United States Forest Service |
Country | United States |
Sector | Academic/University |
PI Contribution | We were based at the Coweeta Field Centre and worked with Coweeta researchers on vegetation sampling. |
Collaborator Contribution | They provided logistical support for fieldwork. |
Impact | 2 papers that are in review currently. |
Start Year | 2013 |
Description | Discovery Channel |
Form Of Engagement Activity | A press release, press conference or response to a media enquiry/interview |
Part Of Official Scheme? | No |
Geographic Reach | International |
Primary Audience | Public/other audiences |
Results and Impact | Short film created for Discovery Channel Canada regarding the initiation of rainfall induced landslides. This was aired in Canada and the USA. |
Year(s) Of Engagement Activity | 2015 |