The AIR Tropical Cyclone Model for India

Similar documents
The AIR Tropical Cyclone Model for Mexico

The AIR Bushfire Model for Australia

The AIR Tropical Cyclone Model for the Carribean

THE AIR SEVERE THUNDERSTORM MODEL FOR AUSTRALIA

AIR Tropical Cyclone Model for the Caribbean

The AIR Severe Thunderstorm Model for the United States

The AIR Crop Hail Model for Canada

THE NEW STORM SURGE MODULE IN AIR S U.S. HURRICANE MODEL

The AIR Hurricane Model for Offshore Assets

Regional Wind Vulnerability. Extratropical Cyclones Differ from Tropical Cyclones in Ways That Matter

Exposure Disaggregation: Introduction. By Alissa Le Mon

AIR Extratropical Cyclone Model for Europe

At the Midpoint of the 2008

The AIR Severe Thunderstorm Model for Europe

Modeling Great Britain s Flood Defenses. Flood Defense in Great Britain. By Dr. Yizhong Qu

AIR Earthquake Model for. Brochure INDIA

A RETROSPECTIVE ON 10 YEARS OF MODELING HURRICANE RISK IN A WARM OCEAN CLIMATE

AIRCURRENTS: EUROPEAN WINDSTORM MODELS: QUESTIONS YOU SHOULD ASK

AIR Extratropical Cyclone Model for Europe

Pacific Catastrophe Risk Assessment And Financing Initiative

The Pressure s On: Increased. Introduction. By Jason Butke Edited by Meagan Phelan

Pacific Catastrophe Risk Assessment And Financing Initiative

The AIR Earthquake Model for Canada

Pacific Catastrophe Risk Assessment And Financing Initiative

AIR Earthquake Model for the PanEuropean Region

KCC White Paper: The 100 Year Hurricane. Could it happen this year? Are insurers prepared? KAREN CLARK & COMPANY. June 2014

Initiative. Country Risk Profile: papua new guinea. Better Risk Information for Smarter Investments PAPUA NEW GUINEA.

Pacific Catastrophe Risk Assessment And Financing Initiative

Long Range Forecast Update for 2014 Southwest Monsoon Rainfall

MODELLING FROST RISK IN APPLE TREE, IRAN. Mohammad Rahimi

Kimberly J. Mueller Risk Management Solutions, Newark, CA. Dr. Auguste Boissonade Risk Management Solutions, Newark, CA

CURRENT AND FUTURE TROPICAL CYCLONE RISK IN THE SOUTH PACIFIC

3. HYDROMETEROLOGY. 3.1 Introduction. 3.2 Hydro-meteorological Aspect. 3.3 Rain Gauge Stations

Comparative Analysis of Hurricane Vulnerability in New Orleans and Baton Rouge. Dr. Marc Levitan LSU Hurricane Center. April 2003

Evidence for Weakening of Indian Summer Monsoon and SA CORDEX Results from RegCM

1990 Intergovernmental Panel on Climate Change Impacts Assessment

AIR Earthquake Model for Japan

The known requirements for Arctic climate services

GC Briefing. Weather Sentinel Hurricane Florence. Status at 5 PM EDT (21 UTC) Today (NHC) Discussion. September 13, 2018

Vulnerability of Bangladesh to Cyclones in a Changing Climate

MODELLING CATASTROPHIC COASTAL FLOOD RISKS AROUND THE WORLD

Colorado State University (CSU) Atlantic Hurricane Season Forecast

5.2 IDENTIFICATION OF HAZARDS OF CONCERN

CURRENT AND FUTURE TROPICAL CYCLONE RISK IN THE SOUTH PACIFIC

Study of Hydrometeorology in a Hard Rock Terrain, Kadirischist Belt Area, Anantapur District, Andhra Pradesh

AIR Earthquake Model for the United States

Improving global coastal inundation forecasting WMO Panel, UR2014, London, 2 July 2014

Global Climate Change, Weather, and Disasters

AIRCURRENTS THE TOHOKU EARTHQUAKE AND STRESS TRANSFER STRESS TRANSFER

Earth Issue: June 2018

Weather Risk Management. Salah DHOUIB Underwriter Paris Re

Global Challenges - Partnering with Service Providers. World Meteorological Organization. J. Lengoasa WMO Deputy Secretary-General

CLIMATE READY BOSTON. Climate Projections Consensus ADAPTED FROM THE BOSTON RESEARCH ADVISORY GROUP REPORT MAY 2016

5.2 IDENTIFICATION OF HAZARDS OF CONCERN

Understanding Climatological Influences on Hurricane Activity: The AIR Near-term Sensitivity Catalog

ovember 2008 Antigua and Barbuda Meteorological Service

Colorado State University (CSU) Atlantic Hurricane Season Forecast

AIRCURRENTS: TRACKING THE 2012 ATLANTIC HURRICANE SEASON USING THE CLIMATECAST U.S. HURRICANE RISK INDEX

Workshop on Drought and Extreme Temperatures: Preparedness and Management for Sustainable Agriculture, Forestry and Fishery

Fire Weather Drivers, Seasonal Outlook and Climate Change. Steven McGibbony, Severe Weather Manager Victoria Region Friday 9 October 2015

Understanding Weather and Climate Risk. Matthew Perry Sharing an Uncertain World Conference The Geological Society, 13 July 2017

N05/3/GEOGR/HP2/ENG/TZ0/XX/Q GEOGRAPHY HIGHER LEVEL PAPER 2. Monday 7 November 2005 (morning) 2 hours 30 minutes INSTRUCTIONS TO CANDIDATES

Geospatial application in Kiribati

EFFECTIVE TROPICAL CYCLONE WARNING IN BANGLADESH

Post-Hurricane Recovery: How Long Does it Take?

Climate Outlook through 2100 South Florida Ecological Services Office Vero Beach, FL September 9, 2014

KUALA LUMPUR MONSOON ACTIVITY CENT

Government of Sultanate of Oman Public Authority of Civil Aviation Directorate General of Meteorology. National Report To

Current Details from the National Hurricane Center (NHC)

P2.57 Cyclone Yasi Storm Surge in Australia Implications for Catastrophe Modeling


UPDATE OF REGIONAL WEATHER AND SMOKE HAZE (December 2017)

Advanced Hydrology. (Web course)

Climate. Annual Temperature (Last 30 Years) January Temperature. July Temperature. Average Precipitation (Last 30 Years)

WMO Statement on the State of the Global Climate Preliminary conclusions for 2018 and WMO Greenhouse Bulletin

New Jersey Department of Transportation Extreme Weather Asset Management Pilot Study

Current Details from the Joint Typhoon Warning Center

Trends in the Character of Hurricanes and their Impact on Heavy Rainfall across the Carolinas

Issued by the: Climate Services Division Fiji Meteorological Service Nadi Airport. 27 October 2010 GENERAL STATEMENT

GIS & Natural Hazards

Study of Changes in Climate Parameters at Regional Level: Indian Scenarios

Thai Meteorological Department, Ministry of Digital Economy and Society

What is the IPCC? Intergovernmental Panel on Climate Change

Effect of land use/land cover changes on runoff in a river basin: a case study

PRMS WHITE PAPER 2014 NORTH ATLANTIC HURRICANE SEASON OUTLOOK. June RMS Event Response

Mozambique. General Climate. UNDP Climate Change Country Profiles. C. McSweeney 1, M. New 1,2 and G. Lizcano 1

ARUBA CLIMATOLOGICAL SUMMARY 2014 PRECIPITATION

Government of India India Meteorological Department (Ministry of Earth Sciences) Subject: Current weather conditions and forecast for next two weeks

5.2 IDENTIFICATION OF HAZARDS OF CONCERN

Complete Weather Intelligence for Public Safety from DTN

Chapter-3 GEOGRAPHICAL LOCATION, CLIMATE AND SOIL CHARACTERISTICS OF THE STUDY SITE

Current Details from the National Hurricane Center (NHC)

Current Details from the National Hurricane Center (NHC)

Natural Disasters in Member Countries (2002 Summary)

JOINT BRIEFING TO THE MEMBERS. El Niño 2018/19 Likelihood and potential impact

Activities and Outlook related to Disaster Reduction in CMA

2013 ATLANTIC HURRICANE SEASON OUTLOOK. June RMS Cat Response

RISK OF PRINCIPAL DISASTERS IN INDIA AND IMPACTS OF DISASTERS ON ECONOMIC DEVELOPMENT

Chiang Rai Province CC Threat overview AAS1109 Mekong ARCC

Intraseasonal Characteristics of Rainfall for Eastern Africa Community (EAC) Hotspots: Onset and Cessation dates. In support of;

Transcription:

The AIR Tropical Cyclone Model for India Tropical cyclones have caused millions, and even billions, of dollars in damage in India. The growing number of properties on the coast, together with growing insurance penetration, make it essential for companies operating in this market to have the tools necessary to make an appropriate assessment of India s tropical cyclone risk and to develop the risk management strategies that will effectively mitigate the impact of the next catastrophe.

Robust Catalog Captures the Full Range of Potential Cyclone Experience The Indian subcontinent divides the North Indian Ocean basin into two seas: the Bay of Bengal to the country s east, and the Arabian Sea to its west. While tropical cyclones take a wide variety of tracks around India, they are four times more likely to originate in the warmer waters of the Bay of Bengal than they are in the Arabian Sea. The AIR Tropical Cyclone Model for India features a catalog of more than 55,000 simulated storms whose wind field and track parameters reflect the full range of potential North Indian Ocean basin cyclones across the entire modeled domain. India s extensive coastline is at risk from both landfalling and bypassing tropical cyclones. Bypassing storms can cause significant damage when they track up long stretches of the coast, delivering damaging winds to coastal exposures and heavy precipitation and flooding hundreds of kilometers inland. The AIR Tropical Cyclone Model for India captures the risk from both wind and flood a critically important feature given that both perils are covered in standard residential and commercial policies. High-Resolution Land Use/Land Cover Data Captures Directional Effects on Surface Wind Speeds To capture surface winds with realism, the model must account for the impact of the surrounding terrain. Winds arriving at a site directly from the Bay of Bengal, for example, will be faster than winds that had to travel first over forested or urban terrain. Using the latest satellite-derived high-resolution land use/land cover and elevation data, the AIR model captures the effects of surface friction on wind speed. It does so for eight wind directions: east, north, northeast, northwest, south, southeast, southwest, and west. Vg Vg wind gradient height wind gradient height Arabian Sea India Bay of Bengal Smooth Terrain (water or open) Rough Terrain (urban or forested) Winds arriving from across the smooth, open ocean will travel faster than winds that have previously traveled across rough or urban terrain. (Source: Cook, 1985) Greater tropical cyclone activity occurs in the Bay of Bengal compared to the Arabian Sea. The AIR cyclone model for India is quite comprehensive and is outstanding for risk evaluation. Dr. A. Meher Prasad, Engineer and India risk expert, peer reviewer of the AIR model. 2

Annual Frequency BI-MODAL CYCLONE SEASON Interrupted by the India Summer Monsoon, the North Indian basin has two peaks in annual tropical cyclone activity: pre-monsoon (May/June) and post-monsoon (October/November). Midsummer monsoon winds propel strong wind shear over the basin, which inhibits tropical cyclone development and intensification. 0.25 0.20 0.15 0.10 0.05 0.00 JANUARY FEBRUARY MARCH APRIL MAY JUNE JULY AUGUST SEPTEMBER OCTOBER NOVEMBER DECEMBER The North Indian Ocean basin exhibits two peaks in the seasonal distribution of tropical cyclone activity. Flood Component Incorporates Detailed Information on Soil Type, Land Use/Land Cover, and Topography Unlike tropical cyclone winds, which generally decrease as a storm moves inland, precipitation intensity and the related flood hazard can actually increase. As such, precipitationinduced flooding can be a major driver of insured loss from India cyclones. The AIR model employs a separate module that is used to determine the spatial distribution of accumulated runoff. Using data about storm size, intensity, and rainfall characteristics, the model captures an hourly precipitation footprint at each location over the entire duration of the storm. Slower moving storms subject locations to higher rainfall totals; thus even weak-wind storms can result in extensive flooding if they have a slow forward speed. The redistribution of rainfall depends on soil type, land use/ land cover, and slope all of which determine what fraction of precipitation is absorbed. If the soil is sandy, a higher fraction will percolate down than if the soil is clay. Similarly, if the land is forested, more precipitation will be absorbed than in a paved urban environment. All else equal, less precipitation will be absorbed on a sloped surface than on one that is flat. The precipitation that is not absorbed is then transported downhill in the direction of the steepest gradient. Leveraging AIR s Detailed Industry Exposure Database for India To generate reliable estimates of industry losses, the AIR model incorporates a comprehensive, high-resolution industry exposure database (IED) that includes residential, commercial and industrial properties. AIR builds the IED by compiling detailed information about risk counts, building attributes and replacement values, as well as information on standard policy terms and conditions from a collection of local sources, including India s Central Statistics Office, the Insurance Regulatory and Development Authority, and the India Central Public Works Department. Because raw exposure data can vary in resolution, AIR employs a sophisticated algorithm to disaggregate all risk counts to a 1-km grid. When detailed, location-specific exposure data is not available, companies can leverage the IED using AIR s detailed modeling capabilities to disaggregate their coarse resolution data to a higher resolution that accurately reflects the spatial distribution of industry exposures. 100-Year Return Period Precipitation < 50 50-100 100-150 150-200 200-250 250-300 300-350 350-400 400-600 > 600 100-Year Return Period Flood < 50 50-100 100-150 150-200 200-250 250-300 300-350 350-400 400-490 Using high-resolution data on land use/land cover, soil type, and topography, the model translates (top) precipitation to (bottom) accumulated runoff, or flood. (Source: AIR) 3

Separate Damage Functions for Wind and Flood Damage functions capture the relationship between the hazard and the vulnerability of affected structures. The model incorporates separate damage functions for the wind and flood perils, as well as by coverage (buildings, contents, and time element); damage functions vary by construction, occupancy, and height. For buildings with unknown construction, occupancy, or height characteristics, the model employs weighted averages of known vulnerability functions based on the regional distribution of these characteristics. For companies with Construction All Risks/Erection All Risks (CAR/EAR) exposures, the model employs damage functions that capture the time-dependent nature of both the vulnerability and replacement cost of buildings under construction. Comprehensive Approach to Model Validation To produce realistic and robust model results, AIR builds its models from the ground up, validating each component independently. For example, the AIR modeled wind speeds and precipitation totals are validated against historical storm data provided by the India Meteorological Department, International Best Track Archive for Climate Stewardship, and Tropical Rainfall Measuring Mission, among other sources. AIR also validates its models from the top down, comparing modeled losses to industry loss estimates and company data. AIR s comprehensive approach to validation confirms that overall losses are reasonable and that the final model output is both consistent with basic physical expectations of the underlying hazard and unbiased when tested against historical and real-time information. 160 Modeled Wind Speeds (Km/h) < 64 64-79 80-99 100-119 120-139 140-159 160-179 180-199 200-220 Okha Bhuj Rajkot Porbandan Keshod Wind Speed (Km/h) 140 120 100 80 60 40 20 Observed Modeled 0 Porbandar Okha Bhuj Rajkot Keshod Modeled wind speeds for the Gujarat cyclone show good agreement with observed maximum wind speed values. (Source: AIR) A COMPONENT-BASED APPROACH TO MODELING COMPLEX INDUSTRIAL FACILITIES The AIR model employs a component-based approach to estimate potential loss from tropical cyclone winds and flooding to complex industrial facilities. AIR assesses the overall vulnerability of over 60 different facility types (e.g., chemical plants, oil refineries) based on the vulnerability of the individual assets the components and sub-components that the facility comprises. The model implicitly accounts for more than 500 distinct industrial components, which have been identified through detailed, site-specific engineering-based risk assessments conducted through AIR s Catastrophe Risk Engineering (CRE) practice. 4

Supports a Wide Array of Policy Terms and Conditions The AIR Tropical Cyclone Model for India supports a wide array of policy terms and conditions, including local limits and deductibles, and policy limits and deductibles. The model takes full advantage of detailed exposure information when available, including the construction, occupancy, age, and height of each structure, locationspecific geographical characteristics (e.g., land use/land cover, elevation, and topography) and geological information (e.g., soil type and permeability). It also takes advantage of local insurance policy and reinsurance treaty terms. Companies with aggregate-level exposure can make use of AIR s high-resolution IED to disaggregate their data for detailed catastrophe analyses. Insured Losses (INR Billion) 30 25 20 15 10 5 0 Orissa Cyclone Modeled Observed 60 50 40 30 20 10 0 Gujarat Cyclone Modeled Observed As a final test in AIR s comprehensive model validation process, modeled losses are compared against reported losses for historical storms at an industry level. Here modeled insured losses are compared against reported losses for the Orissa Cyclone, and for the Gujarat Cyclone, modeled insurable losses are compared to insurable losses derived from reported economic losses. Insurable Losses (INR Billion) Model at a Glance Modeled Perils Supported Geographic Resolution Stochastic and Historical Catalogs Supported Lines of Business Vulnerability Module Tropical cyclone winds and precipitation-induced flood CRESTA/state, district, 6-digit postcode resolution, and can accept user-specified latitude/ longitude Number of events in the stochastic catalog: 35,242 Historical events available: Andhra Pradesh (1990), Gujarat (1998), Orissa (1999) Residential, commercial, industrial, and CAR/EAR Separate wind and flood damage functions for 19 construction types and 114 occupancy classes estimate losses to buildings, contents, and time element coverages. Accounts for the impact of height and year of construction on building vulnerability. Model Highlights For more information regarding AIR s Tropical Cyclone Model for India, please contact your AIR representative. Peer-reviewed model provides coverage for 16 states on the Indian subcontinent, accounting for tropical cyclone activity along both the Arabian Sea and Bay of Bengal coastlines Incorporates the latest land use/land cover data to capture the directional effects of surface friction Explicitly models precipitation-induced flood losses by assessing the accumulated run-off from a storm s precipitation totals Directly accounts for the effect of wind duration on damage Provides separate damage functions for the wind and flood perils, by coverage; damage functions vary by occupancy, construction, and height Damage to large industrial facilities modeled using an objective, engineering-based, component-level approach Supports damage estimation to residential, commercial, and industrial buildings under construction 5

ABOUT AIR WORLDWIDE AIR Worldwide (AIR) provides risk modeling solutions that make individuals, businesses, and society more resilient to extreme events. In 1987, AIR Worldwide founded the catastrophe modeling industry and today models the risk from natural catastrophes, terrorism, pandemics, casualty catastrophes, and cyber attacks, globally. Insurance, reinsurance, financial, corporate, and government clients rely on AIR s advanced science, software, and consulting services for catastrophe risk management, insurance-linked securities, site-specific engineering analyses, and agricultural risk management. AIR Worldwide, a Verisk (Nasdaq:VRSK) business, is headquartered in Boston with additional offices in North America, Europe, and Asia. For more information, please visit www.air-worldwide.com. 2018 AIR Worldwide A Verisk Business