P Termonia, P Willems, N Van Lipzig, J.P. van Ypersele, X Fettweis, K De Ridder, A Gobin, T Stavrakou, P Luyten, S Ponsar, and E Pottiaux (2017)
Combining regional downscaling expertise in Belgium: CORDEX and beyond. Final Report. Belgian Science Policy (BRAIN-be).
Belgian Science Policy.
ABSTRACT
Context
In the context of the Paris Agreement, there exists a clear demand from different stakeholders for
Climate services in Belgium. However, Belgium currently lacks the fundament for enabling such
services.
The CORDEX.be project brought together the Belgian climate and impact modelling research groups
into one network as the first step towards the realization of climate services. It is based on the
international CORDEX (“COordinated Regional Climate Downscaling Experiment”) project but the
“.be” indicates it goes beyond for Belgium.
The key to the foundation of national climate services is a combination of the existing expertise on
high-resolution downscaling, local-impact models, ensemble dynamical and statistical downscaling,
combined with links to international initiatives and stakeholder dialogue. This allows to address the
propagation of climate change and uncertainty from the global to the local scale combined with a
better representation of climate extremes.
The climate network consists of nine partners using four upper-air Regional Climate Models and
seven Local Impact Models. The CORDEX.be framework and guidelines are based on a user-oriented
bottom-up approach.
The CORDEX.be framework provides the first building block for a research network which could be
extended, both nationally and internationally, with the objective of providing climate services.
Objectives
The main objectives of the CORDEX.be project were:
1. Contribute to the international climate community by participating to EURO-CORDEX by
performing regional climate simulations over Europe.
2. Provide an ensemble of High-Resolution (H-Res) climate simulations over Belgium i.e. to
create a small ensemble of high-resolution future projections over Belgium at convection-
permitting resolutions.
3. Couple these model simulation to seven local-impact models for impact studies.
4. Present an overview of the ongoing climate modelling activities in Belgium.
5. Provide coherent climate information for Belgium targeted to end-users, backed by: (i) a
unified framework for the H-Res climate runs and (ii) uncertainty estimations on the climate
change signal;
6. Provide and present a climate-impact report for stakeholders and the general public that
highlight the most important results of the project.
Conclusions
While Belgium does not formally have a national climate centre (Fonteyn, 2013), the CORDEX.be
project provides a platform for data exchange and communication among the Belgian climate-
7Project BR/143/A2/CORDEX.be - Combining regional downscaling expertise in Belgium: CORDEX and beyond
modelling groups. This is coordinated through the website euro-cordex.be. This website will be
maintained and updated with new results and serve as a link between the Belgian activities and the
international ones of the CORDEX project.
In the context of the CORDEX.be project a wide range of climate model simulations has been
performed that are collected on the CORDEX.be data hub at RMI and will serve as the basis of future
impact studies. The model simulations are thoroughly validated by comparison with past
observations and GNSS-derived products.
Different climate impact studies have been performed in the context of CORDEX.be and are
presented here. These include the impact of climate change on
extreme precipitation for Belgium;
maximum snow height for Belgium;
urban parameters for Brussels; including outdoor labor productivity, excess energy
consumption and heat stress due to heat waves;
agricultural crop performance and yield for Belgium;
and biogenic emissions for Europe and Belgium.
Focusing on the future period 2070-2100 for the scenario with the largest greenhouse gas emissions
(RCP8.5), the most prominent impacts of climate change for Belgium include:
A strong increase in tropical days and heat wave days.
An increase in winter precipitation and long extremely wet periods.
Intensification of summer precipitation extremes, especially in urbanized areas. The
precipitation intensity with hourly time scale and 10-year return period may increase up to
100%.
For the Brussels urban environment:
o An increase of a factor 3 to 4 in the number of heat waves.
o Significant increase of heat stress for people living in the city of Brussels, up to twice
as large as in the surrounding rural areas.
o Significant impact on the outdoor productivity due to thermal discomfort. More
specifically, a doubling of lost working days may be expected.
o A doubling of days when air-conditioning is intensively used, impacting the urban
energy consumption.
An increased variability for biomass production and yields. Average yields for fodder maize
and late potatoes will also decline.
Severely reduced winter snow height maxima (above 500m altitude).
An increase of 51% of biogenic emissions from isoprene with the highest emissions in the
Ardennes and Campine forests (disregarding the CO 2 inhibition effect).
Indications exist that there will be less hail events but increase of mean hail size.
8Project BR/143/A2/CORDEX.be - Combining regional downscaling expertise in Belgium: CORDEX and beyond
A table including the climate change numbers and their uncertainty estimates for Belgium are
provided.
Based on interactions and feedback with stakeholders, different applications are planned that
demonstrate the use of the climate data (e.g. Vanderhoeven et al., 2017).
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