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The C3S storm

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Acronyms

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Acronym

Description

C3S

Copernicus Climate Change Service

CDS

Climate Data Store

MLR

Multiple Linear Regression

SIS

Sectoral Information System

WISC

Windstorm Climate Service


Introduction 

Executive Summary

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The C3S storm footprint dataset consists of footprints from all identified winter storms, by the Storm Tracking module, over the period 1979-2021. For those years excluded from the dataset download form, no storms exceeded the selection criteria threshold of 25m/s 10m winds over land using a 3-degree sampling region. Storm footprint are available in NetCDF format. Figure 1 shows an example of the storm footprint for storm Christian which crossed Europe around 28 November 2013, obtained from the statistical downscaling method using the Multiple Linear Regression (MLR) technique, starting from ERA5 model fields.

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Table 1. Overview of key characteristics of the storm footprints.

Data Description


Dataset title

Storm footprint

Data type

Reanalysis post-processed

Topic category

Meteorological geographical feature

Sector

Wind damage

Keyword

Storm footprint.

Dataset language

English

Domain

20W to 35E and from 35N to 70N

Horizontal resolution

Gridded at 1.0km, based on 31km resolution of the ERA5 dataset

Temporal coverage

1979-01-01/to/2021-03-31

Temporal resolution

Maximum 3s wind gust for the 72-hour period is shown at each grid point based on hourly assessments

Vertical coverage

Single level

Update frequency

No updates expected

Version

1.0

Model

ERA5

Experiment

n/a

Provider

KNMI

Terms of Use

https://cds.climate.copernicus.eu/api/v2/terms/static/licence-to-use-copernicus-products.pdf

VariableDescription

 

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Table 2. Overview and description of variables.

Variables




Long Name

Short Name

Unit

Description

Windstorm footprint

-

m s-1

For an identified storm track, the maximum 3- second 10-m wind gust ( m s-1) over the 72-hour period capturing the storm, crossing Europe.
Missing value: -3.4e+38

Input Data

The input data for the statistical downscaling method includes ERA5 10-meter wind gust, wind gusts estimated from the wind-shear between 100 m and 10 m and station elevation height.

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table3
Table 3. Overview of climate model data for input to storm footprint based on statistical downscaling, summarizing the model properties and available scenario simulations.

Input Data





ERA5 wind gust

ECMWF

Scenario

1979-2021

31 km

Windgust
parameterization1

(see footnote)

-

1979-2021

-

Station elevation height

-

-

1979-2021

1 km


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1An effective parametrization of gust profiles during severe wind conditions, Henk W van den Brink, Published 28 November 2019, Environmental Research Communications, Volume 2, Number 1.

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An effective parametrization of gust profiles during severe wind conditions, Henk W van den Brink, Published 28 November 2019, Environmental Research Communications, Volume 2, Number 1.

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This document has been produced in the context of the Copernicus Climate Change Service (C3S).

The activities leading to these results have been contracted by the European Centre for Medium-Range Weather Forecasts, operator of C3S on behalf of the European Union (Delegation

agreement

Agreement signed on 11/11/2014 and Contribution Agreement signed on 22/07/2021). All information in this document is provided "as is" and no guarantee or warranty is given that the information is fit for any particular purpose.

The users thereof use the information at their sole risk and liability. For the avoidance of all doubt , the European Commission and the European Centre for Medium - Range Weather Forecasts have no liability in respect of this document, which is merely representing the author's view.

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