Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Tímea Haszpra"'
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
We address the hypothetical question of whether an increasing total solar irradiance (TSI) trend, without anthropogenic contributions, could be sufficient to explain the ongoing global warming. To this end, the intermediate-complexity climate model P
Externí odkaz:
https://doaj.org/article/653fad3644384cc88129336b9241aceb
Autor:
Tímea Haszpra
Publikováno v:
Atmosphere, Vol 11, Iss 1, p 29 (2019)
Large-scale atmospheric pollutant spreading via volcano eruptions and industrial accidents may have serious effects on our life. However, many students and non-experts are generally not aware of the fact that pollutant clouds do not disperse in the a
Externí odkaz:
https://doaj.org/article/964f5e2475e741b0a563247672afd0bd
Autor:
Tímea Haszpra
Publikováno v:
Atmosphere, Vol 7, Iss 1, p 11 (2016)
Due to the chaotic nature of atmospheric dispersion, small deviations, e.g., numerical errors in dispersion simulations, increase rapidly over time. Therefore, the accuracy of backward simulations is limited. In the paper, the degree of the fulfillme
Externí odkaz:
https://doaj.org/article/553cbb55449f4eeba6f252079b80650a
Autor:
Jonathan L. Mitchell, Qinghua Ding, Tímea Haszpra, Qingquan Li, Rui Luo, Mátyás Herein, Ian Baxter, Dániel Topál
Publikováno v:
Journal of Climate. 33:7431-7454
Arctic sea ice melting processes in summer due to internal atmospheric variability have recently received considerable attention. A regional barotropic atmospheric process over Greenland and the Arctic Ocean in summer (June–August), featuring eithe
Publikováno v:
Journal of Climate. 33:3107-3124
The Arctic Oscillation (AO) and its related wintertime phenomena are investigated under climate change by 2099 in an ensemble approach using the CESM1 Large Ensemble and the MPI-ESM Grand Ensemble with different RCP scenarios. The loading pattern of
Anthropogenic activities contribute to the rising level of greenhouse gas concentrations in the atmosphere at a rate of approximately 1% per year providing a time-dependent external radiative forcing on the climate. In addition to tangible consequenc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d522bd5322729366557e0cda748f4f56
https://doi.org/10.5194/ems2021-404
https://doi.org/10.5194/ems2021-404
Different teleconnection index time series are obtained even within a single member of a large ensemble simulation if different base periods are chosen. This also has an effect on the apparent strength of teleconnections. In this study, the reasons b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1eb1ed92f56059ae19f9a4a71034b1e
https://doi.org/10.5194/egusphere-egu2020-2894
https://doi.org/10.5194/egusphere-egu2020-2894
Autor:
Qinghua Ding, Dániel Topál, Qingquan Li, Tímea Haszpra, Jonathan L. Mitchell, Mátyás Herein, Rui Luo, Ian Baxter
Arctic sea ice melting processes in summer due to internal atmospheric variability have recently received considerable attention. A regional barotropic atmospheric process over Greenland and the Arctic Ocean in summer (June-July-August), featuring ei
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a182abaac6cc5551586de2502ddc50b
https://doi.org/10.5194/egusphere-egu2020-4729
https://doi.org/10.5194/egusphere-egu2020-4729
Traditionally we think that climate is a long term average of weather. It is true but only if the climate is stationary. However, in a changing climate, where one or more relevant system parameters are changing in time, there can be no stationarity b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5095975b3daabbc9566b3804430af19
https://doi.org/10.5194/egusphere-egu2020-7527
https://doi.org/10.5194/egusphere-egu2020-7527