Pregled bibliografske jedinice broj: 1252910
Contributions from Changing Large-Scale Atmospheric Conditions to Changes in Scandinavian Temperature and Precipitation Between Two Climate Normals
Contributions from Changing Large-Scale Atmospheric Conditions to Changes in Scandinavian Temperature and Precipitation Between Two Climate Normals // Tellus A: Dynamic Meteorology and Oceanography, 74 (2022), 2022; 204-221 doi:10.16993/tellusa.49 (međunarodna recenzija, članak, znanstveni)
CROSBI ID: 1252910 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Contributions from Changing Large-Scale
Atmospheric Conditions to Changes in Scandinavian
Temperature and Precipitation Between Two Climate
Normals
Autori
Kjellström, Erik ; Hansen, Felicitas ; Belušić, Danijel
Izvornik
Tellus A: Dynamic Meteorology and Oceanography (1600-0870) 74
(2022), 2022;
204-221
Vrsta, podvrsta i kategorija rada
Radovi u časopisima, članak, znanstveni
Ključne riječi
weather type classification ; circulation type ; climate change ; reanalysis ; Sweden
Sažetak
Multidecadal changes in regional climate can occur as a forced response to changing greenhouse gases and aerosols, as a result of natural internal climate variability, or due to their combination. Internal climate variability is frequently associated with regional changes in large-scale circulation. We investigate how changes in Scandinavian temperature and precipitation conditions during 1961–2020 can be linked to changes in the atmospheric large-scale circulation. The study is based on data from the ERA5 reanalysis and on Swedish average conditions based on observations from the Swedish Meteorological and Hydrological Institute. In general, it is shown that all seasons have become warmer and there is a predominance for more precipitation in the last 30 years. The results also show a clear decrease in daily temperature variability for winter and an increase in summer while there is no similar systematic change for precipitation. Further, we use a circulation type classification technique for identifying ten different circulation types for each calendar month in the 1961–2020 period. Results indicate that changes between the two periods can partly be related to changes in large-scale circulation due to changes in the frequencies of different circulation types. However, it is also clear that the contribution from frequency-related changes to the total change is comparatively low for most months and that changes also within the circulation types are required to explain the total change. The main conclusion of the study is that during the last 30 years it has mostly been warmer than in the preceding 30 years for the same type of weather situation for all months in the year. Consequently, internal climate variability, as represented by changes in the large-scale atmospheric circulation, cannot explain the observed changes in the Scandinavian temperature and precipitation.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika
POVEZANOST RADA
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb
Profili:
Danijel Belušić
(autor)
Citiraj ovu publikaciju:
Časopis indeksira:
- Current Contents Connect (CCC)
- Web of Science Core Collection (WoSCC)
- Science Citation Index Expanded (SCI-EXP)
- SCI-EXP, SSCI i/ili A&HCI
- Scopus