Seasonal Changes in Solar Radiation and Relative Humidity in Europe in Response to Global Warming

• Published in: Journal of climate 2013-04, Vol.26 (8), p.2467-2481
• Main Authors: Ruosteenoja, Kimmo, Räisänen, Petri
• Format: Article
• Language: English
• Subjects: 21st century; Atmosphere; Climate change; Climate models; Climatology. Bioclimatology. Climate change; Computer simulation; Drought; Earth, ocean, space; Energy consumption; Exact sciences and technology; External geophysics; Global climate models; Global warming; Greenhouse gases; Humidity; Intercomparison; Mathematical models; Mental health; Meteorology; Modeling; Moisture effects; Oceans; Peninsulas; Precipitation; Radiation; Relative humidity; Seasonal variation; Seasonal variations; Seasons; Simulation; Simulations; Solar radiation; Solar temperature; Summer; Temperature; Trends; Winter
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-12-00007.1

Future seasonal changes in surface incident solar radiation and relative humidity (RH) over Europe and adjacent ocean areas were assessed based on phase 3 of the Coupled Model Intercomparison Project (CMIP3) model ensemble. Under the A1B scenario, by 2070–99, summertime solar radiation is projected to increase by 5%–10% in central and southern Europe. In winter, radiation decreases in most of northern and eastern Europe by 5%–15%. RH drops in summer in the southern European inland by 8%–12%, whereas in winter a small increase of 2%–3% is projected for northeastern Europe. In spring, the change is an intermediate between those in the extreme seasons, while in autumn the patterns resemble summer. Over the northern Atlantic Ocean, RH increases in all seasons by 1%–2%. The intermodel agreement on the sign of all these shifts is good, and the patterns recur in the responses to the A2 and B1 scenarios. Substantial changes are already simulated to occur before the midcentury, for example, in summer RH decreases by more than 5% in the inner Balkan Peninsula. Projected changes in these two variables agree well and are also mainly consistent with precipitation responses both in the multimodel mean and in individual models. According to all indicators, southern European summers become more arid, while winters, in the north particularly, become moister and darker. The increasing radiation and declining RH exacerbate summertime drought in southern Europe, whereas excessive humidity in the north may, for example, inflict moisture damages in constructions.