Covered Area Rainfall Event (9 November 2015) Excess Rainfall

Similar documents
Covered Area Rainfall Event (26 February 2016) Excess Rainfall

Covered Area Rainfall Event (29-30 September 2016) Tropical Cyclone Matthew Excess Rainfall

Covered Area Rainfall Event (28-30 September 2016) Tropical Cyclone Matthew Excess Rainfall

Covered Area Rainfall Event (18-20 October 2017) Excess Rainfall

Covered Area Rainfall Event (18-19 September 2017) Hurricane Maria Excess Rainfall

Haiti. Excess Rainfall. Covered Area Rainfall Events (19 & 23 September 2014)

Tropical Cyclone EARL (AL052016)

Covered Area Rainfall Event (5-8 October 2017) Tropical Storm Nate Excess Rainfall

Tropical Cyclone Harvey (AL092017)

Tropical Cyclone Joaquin (AL112015)

Tropical Cyclone Isaac (AL092012)

Tropical Cyclone Gonzalo (AL082014)

Tropical Cyclone Sandy (AL182012)

Revealing the interaction between Society and Nature. DesInventar, disaster inventories for damage and loss assessment

Ms. Latoya Regis. Meteorologist Hydrometeorological Service, Guyana

Disaster Risk Assessment: Opportunities for GIS and data management with Open DRI

Caribbean Early Warning System Workshop

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

HYDRO-METEOROLOGICAL INVESTIGATION OF 2015 FLASH FLOOD IN EASTERN HILL BASIN BANGLADESH

Billion Dollar U.S. Flood Disasters in 2016

Seasonal prediction of extreme events

The Impact of 2007 Atlantic Hurricane Season on Dominica

Weather Risk Management. Salah DHOUIB Underwriter Paris Re

Severe Weather Watches, Advisories & Warnings

L alluvione di Firenze del 1966 : an ensemble-based re-forecasting study

Flash Flood Guidance System On-going Enhancements

Belize Country Report Status, Advances, and Needs. Rudolph Williams and Eden Garcia Hydrology Unit/University of Belize 2/18/2009

US/Global Natural Catastrophe Update

Copernicus Overview. Major Emergency Management Conference Athlone 2017

C o p e r n i c u s E m e r g e n c y M a n a g e m e n t S e r v i c e f o r e c a s t i n g f l o o d s

Evaluation of Flash flood Events Using NWP Model and Remotely Sensed Rainfall Estimates

Cambridge International Examinations Cambridge International General Certificate of Secondary Education

Global Flash Flood Forecasting from the ECMWF Ensemble

MODELLING FROST RISK IN APPLE TREE, IRAN. Mohammad Rahimi

Weather Derivatives-Pricing and Design Issue in India

What Are Disasters? The Rescue Kids Trio!

Landslide Disaster Management in Sri Lanka and Nichola Oya as a Case study. Group 16 Gamini Jayathissa Udeni Nawagamuwa

Assessment of the catastrophic events originated in the river Vere basin

Overview and purposes of the meeting

Striving Sufficient Lead Time of Flood Forecasts via Integrated Hydro-meteorological Intelligence

NOAA s National Weather Service Philadelphia/Mt. Holly NJ

Africa RiskView MONTHLY BULLETIN JANUARY Highlights: Rainfall

Impact on Agriculture

Word Cards. 2 map. 1 geographic representation. a description or portrayal of the Earth or parts of the Earth. a visual representation of an area

ENGINEERING HYDROLOGY

Floods. Floods COMMUNITY EMERGENCY RESPONSE TEAM FLOODS CONTENT INSTRUCTOR GUIDANCE

Climate Indices and Indicators for Agriculture

SEVERE WEATHER 101. Flood Basics

COASTAL HAZARDS. Alan Lulloff, Water Management Engineer Wisconsin Department of Natural Resources. Local Contact: John Spangberg (715)

Involvement of the Geological Survey of Slovenia in the field of natural hazard risk management

GENERAL. CHAPTER 1 BACKGROUND AND PURPOSE OF THE GUIDELINES Background of the Guidelines Purpose of the Guidelines...

Smart use of Geographic Information System (GIS) platform for delivering weather information and nowcasting services

California OES Weather Threat Briefing

Development of Tropical Storm Falcon (Meari) over the Philippines

High Rainfall Events and Their Changes in the Hawaiian Islands

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

Daily Operations Briefing. Monday, July 10, :30 a.m. EDT

Untitled.notebook May 12, Thunderstorms. Moisture is needed to form clouds and precipitation the lifting of air, or uplift, must be very strong

April Forecast Update for North Atlantic Hurricane Activity in 2019

Outline. Remote Sensing, GIS and DEM Applications for Flood Monitoring. Introduction. Satellites and their Sensors used for Flood Mapping

SECTION II Hydrological risk

A Preliminary Severe Winter Storms Climatology for Missouri from

The AIR Severe Thunderstorm Model for the United States

Cataloguing high impact Weather and Climate Events

Catastrophic Events Impact on Ecosystems

8 Current Issues and Research on Sediment Movement in the River Catchments of Japan

17 th Session of RA IV

Analysis of catastrophic floods affecting Croatia in May 2014 Meteorological and Hydrological Service Zagreb, Croatia

Souris River Basin Spring Runoff Outlook As of March 15, 2018

Integrating Hydrologic and Storm Surge Models for Improved Flood Warning

GIS as a tool in flood management

April Forecast Update for Atlantic Hurricane Activity in 2018

COMMUNITY EMERGENCY RESPONSE TEAM FLOODS INTRODUCTION

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

FFGS Advances. Initial planning meeting, Nay Pyi Taw, Myanmar February, Eylon Shamir, Ph.D,

Dr Harvey Stern. University Of Melbourne, School Of Earth Sciences

VINCENT COOPER Flood Hazard Mapping Consultant

EFFECTS OF GLOBAL WARMING ON LANDSLIDE FREQUENCIES IN RATNAPURA DISTRICT, SRI LANKA- 2011

Weather briefing Strong Coastal Nor easter November 7 th -8 th, 2012

Calibrating forecasts of heavy precipitation in river catchments

PROF. DR HAB. PIOTR TRYJANOWSKI

DEVELOPMENT OF CARIBBEAN RISK ATLAS FOR EARTHQUAKE HAZARDS (RISK ATLAS PROJECT)

FEMA Hazards Loss Modeling Task Force (MOTF) Situation Report #14. Colorado Spring Flood Risk ***FINAL REPORT***

Innovative Ways to Monitor Land Displacement

The Effects of Hydraulic Structures on Streams Prone to Bank Erosion in an Intense Flood Event: A Case Study from Eastern Hokkaido

Global Flash Flood Guidance System Status and Outlook

Rainfall Prediction System for the CuaDat Dam Basin

Appendix 1: UK climate projections

IWT Scenario 2 Integrated Warning Team Workshop National Weather Service Albany, NY October 31, 2014

GIS in Weather and Society

Science of Natural Disasters: RIVERS& FLOODS! 27 April 2016

AHEAD OF THE STORM: Extreme Weather Resilience in the City of Toronto

Haiti and Dominican Republic Flash Flood Initial Planning Meeting

EIT-Japan Symposium 2011 on Human Security Engineering

BRITISH VIRGIN ISLANDS HURRICANE SEASON REPORT JUNE 2017 PRESENT

International Flood Network - IFNet

3.1. The Climatological Relation Between Extreme Precipitable Water Vapor (PWV) and Precipitation for the September 2013 Colorado Flooding Event

Trend of Annual One-Day Maximum Rainfall Series over South India

H.3 Severe Impacts of Hurricane Irma in Cuba: Forecast Models, Forecast and Warning Processes.

FLOOD HAZARD AND RISK ASSESSMENT IN MID- EASTERN PART OF DHAKA, BANGLADESH

Transcription:

Covered Area Rainfall Event (9 November 2015) Excess Rainfall Event Briefing 17 November 2015 Vito Alessio Robles No.179. Col. Hda Gpe Chimalistac. Del. Álvaro Obregón. Cp 01050, México D.F. Tel: +52 (55) 5616-8161, 62, 64 www.ern.com.mx

1 INTRODUCTION The Caribbean Rainfall Model (operated by Kinetic Analysis Corporation (KAC)) indicated that a Covered Area Rainfall Event (CARE) was generated in Grenada starting and ending on 9 November 2015. 2 RAINFALL MODEL OUTPUTS The Caribbean Rainfall Model uses a 2-day running aggregate of rainfall measurements for Grenada, meaning that the rainfall attributed to a particular day is the total sum of the rainfall on that day itself and the following day. For the 9 November CARE, the Caribbean Rainfall Model reported a Maximum Aggregate Rainfall of 112 mm in St. Mary, in the centre of the island (Figure 1) and the maximum number of ongoing WRFXSR Grid Cells Events was 388. 3 TRIGGER POTENTIAL The number of ongoing Grid Cells Events exceeded the required threshold (273) to trigger the CARE on 9 November and fell below the threshold the next day. While the CARE technically lasted only one day, a CARE is not considered complete until the Aggregate Rainfall in each WRFXSR Grid Cell (that had an ongoing WRFXSR Grid Cell Event that contributed to the CARE) has fallen below 50 mm for at least 2 days. The CARE was considered complete on 10 November 2015. The Rainfall Index Loss calculated for this CARE was zero and therefore no payout is due. 4 IMPACTS According to information provided by the Grenada National Disaster Coordinator, Mr. Terence Walters, the rainfall event caused minor damage as follows: two rivers overflowed their banks, two schools were flooded and had to remain closed for one day, several landslides and rock falls occurred, flash floods caused damage to some crops, and one wooden house was partially destroyed due to land slippage. 2

Figure 1. Map showing accumulated rainfall in Grenada, 9 November 2015. For further information, please contact ERN-RED, the CCRIF SPC Risk Management Specialist. Evaluación de Riesgos Naturales Vito Alessio Robles No.179 Col. Hda Gpe Chimalistac. Del. Álvaro Obregón. Cp 01050, México D.F. +52 (55) 5616-8161, 62, 64 cavelar@ccrif.org 3

DEFINITIONS Active Percentage Aggregate Rainfall The percentage of the total number of WRFXSR 1 Grid Cells, within the Covered Area of the Insured, in which a WRFXSR Grid Cell Event must be occurring to trigger a Covered Area Rainfall Event. The Active Percentage is defined in the Schedule. The value of Aggregate Rainfall, as measured in millimeters (mm), using the WRFXSR Precipitation Data over the Covered Area and evaluated by the Calculation Agent as part of the Rainfall Index Loss Calculation Methodology. For a given day: (a) 2-day aggregate - the total sum of rainfall on the day itself, and the day after; or (b) 3-day aggregate - the total sum of rainfall on the day itself, and the two following days. Caribbean Rainfall Model Covered Area Rainfall Event Covered Area WRFXSR Grid Cell (grid cell) The computer model used to calculate the WRFXSR Grid Cell Event Loss and the Rainfall Index Loss. Any continuous period of days during which the number of WRFXSR Grid Cell Events is greater than or equal to the product of (a) Active Percentage multiplied by (b) the total number of WRFXSR Grid Cells within the Covered Area. The territory of the Insured as represented in the Caribbean Rainfall Model. The 30 arc-second by 30 arc-second grid of cells each of which is attributed with an exposure value and, for those with exposure value greater than zero, to which an Aggregate Rainfall Amount is attributed each day. WRFXSR Grid Cell Event (cell event) Any continuous period of days during which the Aggregate Rainfall value equals or exceeds the Rainfall Event Threshold in a WRFXSR Grid Cell. For Covered Areas that have 3-day aggregation periods, a WRFXSR Grid Cell Event is only considered to be over once there have been 1 Weather Research and Forecasting (WRF) Excess Rainfall (XSR) 4

two or more consecutive days where the Aggregate Rainfall does not exceed the Rainfall Event Threshold. Maximum Aggregate Rainfall Rainfall Event Threshold Rainfall Index Loss The highest Aggregate Rainfall amount during a WRFXSR Grid Cell Event for each WRFXSR Grid Cell in which there is a WRFXSR Grid Cell Event. Aggregate Rainfall level which, when exceeded, starts a WRFXSR Grid Cell Event. For any Covered Area Rainfall Event affecting the Insured, the US Dollar loss calculated by the Calculation Agent using the Caribbean Rainfall Model. 5