Pregled bibliografske jedinice broj: 1212729
Impact of tropical SSTs on the variability and predictable components of late-winter atmospheric circulation in the North Atlantic-European region
Impact of tropical SSTs on the variability and predictable components of late-winter atmospheric circulation in the North Atlantic-European region // EMS Annual Meeting Abstracts, Vol. 19
Bonn, Njemačka, 2022. str. 208-208 doi:10.5194/ems2022-208 (predavanje, međunarodna recenzija, sažetak, znanstveni)
CROSBI ID: 1212729 Za ispravke kontaktirajte CROSBI podršku putem web obrasca
Naslov
Impact of tropical SSTs on the variability and predictable components of late-winter atmospheric circulation in the North Atlantic-European region
Autori
Ivasić, Sara ; Herceg Bulić, Ivana
Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni
Izvornik
EMS Annual Meeting Abstracts, Vol. 19
/ - , 2022, 208-208
Skup
EMS Annual Meeting 2022
Mjesto i datum
Bonn, Njemačka, 04.09.2022. - 09.09.2022
Vrsta sudjelovanja
Predavanje
Vrsta recenzije
Međunarodna recenzija
Ključne riječi
Climate variability ; North Atlantic-European climate ; Tropical-extratropical teleconnections ; Boundary-forced predictability
Sažetak
Atmospheric variability and predictable components over the North Atlantic-European region (NAE) were analysed in the late-winter season using a general circulation model of intermediate complexity (ICTP AGCM). The method of empirical orthogonal functions (EOF) analysis was applied to 200-hPa geopotential heights (GH200) to extract individual modes of variability occurring in the ensemble of numerical simulations. The same variable was selected for the signal-to-noise optimal patterns method, which identifies the patterns maximising the signal-to-noise ratio, following Straus et al. (2003). Six experiments based on a 35-member ensemble of 156-year long simulations were conducted to detect the potential impact of tropical sea surface temperatures. Each experiment was forced with observed sea surface temperature anomalies prescribed in different ocean areas: globally, in the tropics, in the tropical Atlantic region, in the tropical Pacific, and the tropical Indian Ocean. In late winter, the leading EOF pattern calculated for all individual ensemble members projects onto the North Atlantic Oscillation, while the second EOF pattern projects onto the East Atlantic pattern. However, EOF modes based on the ensemble mean, which should reflect the forced component of the signal, have different spatial characteristics. Alongside the classical analysis of signal and noise, results of the signal-to-noise optimal patterns method suggest that the optimal patterns and signal-to-noise ratio are affected by the boundary forcing of the oceans. Relatively high correlations between the first principal component of NOAA SST anomalies in different ocean basins and the principal components of GH200, as well as with the time series of the first optimal pattern, further confirm the connection between remote SSTs and potential predictability of the GH200 over the NAE region in late winter. Furthermore, the resemblance between the first optimal pattern and the EOF1 pattern based on the ensemble mean points toward the vital role of the lower-boundary-forced signal in establishing potential predictability in the NAE region.
Izvorni jezik
Engleski
Znanstvena područja
Geofizika
POVEZANOST RADA
Projekti:
HRZZ-UIP-2017-05-6396 - Klimatske promjene i varijabilnost u Hrvatskoj – od globalnih utjecaja do lokalnih zelenih rješenja (CroClimGoGreen) (Herceg Bulić, Ivana, HRZZ - 2017-05) ( CroRIS)
Ustanove:
Prirodoslovno-matematički fakultet, Zagreb