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Dataset

 

Met Office Wind-Driven Rain (WDR)

Latest Data Update: 2025-02-12
Status: Completed
Online Status: ONLINE
Publication State: Citable
Publication Date: 2025-01-09
DOI Publication Date: 2025-01-20
Download Stats: last 12 months
Dataset Size: 39 Files | 1001MB

Abstract

This dataset contains the annual index of wind-driven rain (sum of all wind-driven rain spells in each year) derived from the UK Climate Projections (UKCP18) for a range of future global warming levels provided on a 5 km British National Grid (BNG). The annual index is calculated for eight wall orientations corresponding to the cardinal and ordinal points of the compass.

Wind-driven rain occurs when falling rain is blown by a horizontal wind so that it falls diagonally towards the ground. The annual index of wind-driven rain is the sum of all wind-driven rain spells for a given wall orientation and time period. It’s measured as the volume of rain blown from a given direction in the absence of any obstructions, with units of litres per square metre per year.

Wind-driven rain is calculated from hourly weather and climate data using an industry-standard formula from ISO 15927–3:2009, which is based on the product of wind speed and rainfall totals. Wind-driven rain is only calculated if the wind would strike a given wall orientation. A wind-driven rain spell is defined as a wet period separated by at least 96 hours with little or no rain (below a threshold of 0.001 litres per m2 per hour).

The annual index of wind-driven rain is calculated for a baseline (historical) period of 1981-2000 (corresponding to 0.61°C warming) and for global warming levels of 2.0°C and 4.0°C above the pre-industrial period (defined as 1850-1900). The warming between the pre-industrial period and baseline is the average value from six datasets of global mean temperatures available on the Met Office Climate Dashboard: https://climate.metoffice.cloud/dashboard.html.

The magnitudes of 1 in 3 year wind-driven rain spells (i.e. wet spells that would be expected to occur, on average, once every three years) are used to divide the UK into four zones in Approved Document C of the buildings regulations. The magnitudes of 1 in 3 year wind-driven rain spells were calculated for the baseline period (1981-2000) and 20-year periods corresponding to 2°C and 4°C of warming. The magnitudes of all wet spells (here, sum of hourly values of the wind-driven rain metric, I) were calculated, and the largest wet spell in each year was found (in the accompanying report, the magnitude of a wet spell is given the symbol Is' ["Is prime"] and has units of litres per metre-squared per spell). For each time period, the largest spells in all years and ensemble members were pooled together. A Gumbel distribution was fitted to the pooled data and used to estimate the magnitude of the 1 in 3 year wet spells across the UK.

Wind-driven rain is required for buildings standards. It is a major source of moisture in walls. Areas subject to very high levels of wind-driven rain may not be suitable for cavity-wall insulation. Under certain circumstances, cavity-wall insulation can enhance the transfer of moisture through walls to the inside of a building causing mould and damp problems.

Citable as:  Sanderson, M.; Eastman, M.; Neto-Bradley, A.; Lowe, J. (2025): Met Office Wind-Driven Rain (WDR). NERC EDS Centre for Environmental Data Analysis, 20 January 2025. doi:10.5285/3acecae819b84507ad4d62f87cf35155. https://dx.doi.org/10.5285/3acecae819b84507ad4d62f87cf35155

Abbreviation: Not defined
Keywords: wind-driven rain, Met Office, UKCP18, DESNZ

Details

Previous Info:
No news update for this record
Previously used record identifiers:
No related previous identifiers.
Access rules:
Public data: access to these data is available to both registered and non-registered users.
Use of these data is covered by the following licence(s):
http://www.nationalarchives.gov.uk/doc/open-government-licence/version/3/
When using these data you must cite them correctly using the citation given on the CEDA Data Catalogue record.
Data lineage:

Wind-driven rain was derived from hourly climate data produced as part of the UKCP18 Local climate projections. Data were produced by the project team and supplied for archiving at the Centre for Environmental Data Analysis (CEDA).

Data Quality:
The data produced were compared with previously published values and those derived from weather stations.
File Format:
The data are provided in NetCDF.

Process overview

This dataset was generated by the computation detailed below.
Title

Computation for Wind-Driven Rain

Abstract

Wind-driven rain is calculated from hourly weather and climate data using an industry-standard formula from ISO 15927–3:2009, which is based on the product of wind speed and rainfall totals. Wind-driven rain is only calculated if the wind would strike a given wall orientation. A wind-driven rain spell is defined as a wet period separated by at least 96 hours with little or no rain (below a threshold of 0.001 litres per m2 per hour).

The annual index of wind-driven rain is calculated for a baseline (historical) period of 1981-2000 (corresponding to 0.61°C warming) and for global warming levels of 2.0°C and 4.0°C above the pre-industrial period (defined as 1850-1900). The warming between the pre-industrial period and baseline is the average value from six datasets of global mean temperatures available on the Met Office Climate Dashboard: https://climate.metoffice.cloud/dashboard.html.

The magnitudes of 1 in 3 year wind-driven rain spells (i.e. wet spells that would be expected to occur, on average, once every three years) were calculated for the baseline period (1981-2000) and 20-year periods corresponding to 2°C and 4°C of warming. The magnitudes of all wet spells (here, sum of hourly values of the wind-driven rain metric, I) were calculated, and the largest wet spell in each year was found (in the accompanying report, the magnitude of a wet spell is given the symbol Is' ["Is prime"] and has units of litres per metre-squared per spell). For each time period, the largest spells in all years and ensemble members were pooled together. A Gumbel distribution was fitted to the pooled data and used to estimate the magnitude of the 1 in 3 year wet spells across the UK.

Input Description

None

Output Description

None

Software Reference

None

  • var_id: annual_index_of_wind_driven_rain
  • long_name: Annual index of wind-driven rain
  • units: litres m-2 year-1
  • var_id: magnitude_of_1_in_3_year_events
  • long_name: Magnitude of 1 in 3 year events
  • units: litres m-2
  • var_id: wd_names
  • long_name: Wall direction names
  • units: 1
  • long_name: ensemble_member
  • var_id: ensemble_member
  • units: 1
  • long_name: ensemble_member_id
  • var_id: ensemble_member_id
  • units: m
  • standard_name: projection_x_coordinate
  • var_id: projection_x_coordinate
  • var_id: projection_x_coordinate_bnds
  • units: m
  • standard_name: projection_y_coordinate
  • var_id: projection_y_coordinate
  • var_id: projection_y_coordinate_bnds
  • var_id: time_bnds
  • var_id: transverse_mercator
  • units: degrees
  • var_id: wall_orientation
  • long_name: wall_orientation

Co-ordinate Variables

  • units: degrees_north
  • standard_name: latitude
  • var_id: latitude
  • units: degrees_east
  • standard_name: longitude
  • var_id: longitude
  • standard_name: time
  • var_id: time
  • units: hours
Coverage
Temporal Range
Start time:
1980-12-01T00:00:00
End time:
2077-11-01T23:59:59
Geographic Extent

 
60.5300°
 
-12.8000°
 
3.4100°
 
49.3100°