First look at changes in flood hazard in the Inter-Sectoral Impact Model Intercomparison Project ensemble
Rutger Dankers1, Nigel W Arnell, Douglas B Clark
1Met Office Hadley Centre, Exeter EX1 3PB, United Kingdom.
Summary
Climate change will increase global flood risk, with many regions experiencing more frequent 30-year flood peaks. However, some areas, especially those with snowmelt-driven rivers, may see decreased flood hazard due to changing precipitation patterns.
Area of Science:
- Environmental science
- Climate science
- Hydrology
Background:
- Anthropogenic greenhouse gas emissions drive climate change, altering precipitation patterns.
- Increased precipitation intensity and frequency are expected, potentially raising future flood probabilities.
- Global flood hazard assessments are crucial for understanding climate change impacts.
Purpose of the Study:
- To explore uncertainties in global flood hazard projections under climate change.
- To analyze changes in the 30-year return level of 5-day average peak river flows.
- To assess impacts using the Representative Concentration Pathway RCP8.5 scenario for the end of the century.
Main Methods:
- Utilized river flow simulations from nine global hydrology and land surface models.
- Analyzed changes in the 30-year return level of 5-day average peak flows.
- Evaluated flood hazard under the RCP8.5 climate change scenario.
Main Results:
- Climate change is projected to increase flood hazard frequency at over half of global land grid points.
- Decreased flood hazard magnitude and frequency are predicted for approximately 20-45% of land grid points, particularly snowmelt-dominated regions.
- The current 30-year flood peak is projected to occur more frequently (more than once every 5 years) across 5-30% of land grid points.
Conclusions:
- Large-scale patterns of flood hazard change are consistent across models, but local-scale projections show significant uncertainty.
- Model uncertainty, even on the sign of change, is substantial at the river basin scale.
- Acknowledging and incorporating modeling uncertainties is vital for local flood adaptation studies.
Related Concept Videos
Design Example: Analyzing Capacity Contours for Flood Risk Assessment
391
Flood risk assessment involves careful planning and analysis to ensure the safety of communities near water retention structures. Capacity contours are a vital tool in this process, as they illustrate the potential spread of water at specific levels in a given area. In the context of building a bund across a small valley, these contours play a critical role in evaluating the safety of nearby residential areas.In this example, the bund is intended to store stormwater in the valley. The engineers...
391
Applications of GIS: Disaster Management and Emergency Response
773
Geographic Information System (GIS) technology is essential for risk identification, action prioritization, and resource optimization in critical situations like flooding and earthquakes. By integrating spatial and demographic data, GIS provides a comprehensive framework for emergency response.GIS integrates data layers, like rainfall intensity, topography, elevation profiles, and river levels, to model high-risk flood zones. These layers assess areas susceptible to flooding based on their...
773
Responses to Drought and Flooding
10.2K
Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
10.2K
Hazard Rate
525
The hazard rate, also known as the hazard function or failure rate, is a statistical measure used to describe the instantaneous rate at which an event occurs, given that the event has not yet happened. From a probabilistic perspective, it represents the likelihood that a subject will experience the event in a very small time interval, conditional on surviving up to the beginning of that interval. In terms of frequency, the hazard rate can be viewed as the ratio of the number of events to the...
525
Precipitation and Co-precipitation
4.8K
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
4.8K
Precipitation Processes
5.0K
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
5.0K


