Nalazite se na CroRIS probnoj okolini. Ovdje evidentirani podaci neće biti pohranjeni u Informacijskom sustavu znanosti RH. Ako je ovo greška, CroRIS produkcijskoj okolini moguće je pristupi putem poveznice www.croris.hr
izvor podataka: crosbi !

Climate change impact on future heating and cooling needs in Osijek (Croatia) (CROSBI ID 671067)

Prilog sa skupa u zborniku | sažetak izlaganja sa skupa | međunarodna recenzija

Cvitan, Lidija ; Patarčić, Mirta Climate change impact on future heating and cooling needs in Osijek (Croatia). 2018

Podaci o odgovornosti

Cvitan, Lidija ; Patarčić, Mirta

engleski

Climate change impact on future heating and cooling needs in Osijek (Croatia)

Osijek is the largest city of eastern Croatia. Osijek is situated in Drava River lowland in Pannonian basin, with continental climate which is usually characterised by hot summers and cold winters. That is the consequence of rather weak maritime influence of the Mediterranean in this Croatian area. Therefore, heating and cooling needs were there among the greatest in Croatia until now. Investigation of impact of climate change on heating and cooling needs in Osijek in future is continued using the commonly used degree-days method. Only heating degree-day (HDD) for the whole heating season (October-April) and cooling degree-day (CDD) for the whole cooling season (May-September) were analyzed. For two future periods, 2011-2040 (P1) and 2041-2070 (P2), mean daily temperature input data were achieved by means of a subset of nine regional climate models from the EU FP6 ENSEMBLES project. Horizontal resolution of each model was 25 km and models’ projections were performed under the assumption of A1B greenhouse gases emission scenario. Future projections of heating and cooling parameters for Osijek station were determined by using simulated 2-m air temperatures from the model grid point which is closest to the station. As heating and cooling degree-days are temperature parameters, it is important to know how well the simulated temperature compares against observation data. For that reason nine temperature biases (model minus observations) averaged over three periods over the year (January-April, May-September and October-December) for the 1961-1990 (P0) control period were determined. For the same control period, nine simulations of heating and cooling degree-days were also calculated. Comparison of the degree-day simulations with temperature biases over the control period helped in detecting the simulations that are closest to the observations (i.e. the most realistic simulations). For P1 and P2 future climates, projected degree-day trends are shown. For both future periods the most realistic simulations show decreasing HDD trends and increasing CDD trends.

projected degree-day trends ; models from the EU FP6 ENSEMBLES ; A1B scenario ; periods 2011-2040 and 2041-2070

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

nije evidentirano

Podaci o prilogu

EMS2018-425

2018.

objavljeno

Podaci o matičnoj publikaciji

Podaci o skupu

European Conference for Applied Meteorology and Climatology 2018 ; Weather and climate: global change and local hazards

poster

03.09.2018-07.09.2018

Budimpešta, Mađarska

Povezanost rada

Geofizika

Poveznice