Suchergebnisse

ONE CANNOT FULLY UNDERSTAND THE ORIGINS OF THE 1956 HUNGARIAN REVOLUTION WITHOUT TAKING INTO ACCOUNT THE YUGOSLAV CONNECTION. THIS ARTICLE ILLUMINATES THE BEHAVIOR OF TITO AND HIS SUBORDINATES IN THE 1956 EVENTS, DRAWING ON NEWLY RELEASED DOCUMENTS FROM FOUR OF MOSCOW'S MAJOR ARCHIVES, INCLUDING THE SECRET NOTES OF KEY CPSU PRESIDIUM MEETINGS. IT ALSO EXPLAINS THE HITHERTO MURKY CIRCUMSTANCES SURROUNDING TITO'S DECISION TO GRANT IMRE NAGY POLITICAL REFUGE IN HIS BUDAPEST EMBASSY ON THE DAY ON THE INVASION. IT IS ARGUED THAT HAD IT NOT BEEN FOR THE SINO-SOVIET DISPUTE OF THE EARLY 1960S, THE EVENTS OF 1956 MIGHT HAVE LED TO ANOTHER COMPLETE BREAK BETWEEN YUGOSLAVIA AND THE BLOC COUNTRIES CLOSEST TO THE USSR.

Comparisons between satellite and ground-based measurements of the atmosphere are inevitably affected by natural variability due to mismatches in spatial and temporal co-location. These additional terms in the comparison error budget are quantified here for total ozone column comparisons using an Observing System Simulation Experiment. Even when using tight co-location criteria, atmospheric variability is found to impact the comparisons significantly. ; Part of this work was funded by the Belgian Science Policy Office (BELSPO) and ESA via the ProDEx projects A3C and ACROSAT, and by the EU H2020 project GAIA-CLIM (Ares(2014)3708963/Project 640276). The authors acknowledge the pioneering research carried out in 2008–2012 by C. De Clercq and S. Vandenbussche and funded by the EU FP6 project GEOmon (FP6-2005-Global-4-036677) and ProDEx project SECPEA.

Comparisons between satellite and ground-based measurements of the atmosphere are inevitably affected by natural variability due to mismatches in spatial and temporal co-location. These additional terms in the comparison error budget are quantified here for total ozone column comparisons using an Observing System Simulation Experiment. Even when using tight co-location criteria, atmospheric variability is found to impact the comparisons significantly. ; Part of this work was funded by the Belgian Science Policy O ce (BELSPO) and ESA via the ProDEx projects A3C and ACROSAT, and by the EU H2020 project GAIA-CLIM (Ares(2014)3708963/Project 640276). Finally, the 20 authors acknowledge the pioneering research carried out in 2008–2012 by C. De Clercq and S. Vandenbussche and funded by the EU FP6 project GEOmon (FP6-2005-Global-4-036677) and ProDEx project SECPEA.