Abstract
The current research aims at studying the spatio-temporal distribution of blocking events in the Northern and Southern Hemispheres from 1968 to 2018, for a period of 51 years based on the Wiedenmann block intensity (BI) index. The results showed that blocking events in the Northern Hemisphere are almost twice as often as in the Southern Hemisphere. This could be due to the uneven distribution of land and water areas, and resulted from the greater temperature differences in the Northern Hemisphere. Blockings in the Northern Hemisphere are also stronger than in the Southern Hemisphere in terms of intensity, strength, and durability. The reason can be attributed to the greater temperature difference between water and land in the Northern Hemisphere. In terms of seasonal occurrence of blockings, the highest frequency of blockings in the Northern Hemisphere is related to spring in the North Atlantic and in the Southern Hemisphere, it is related to winter in the South Atlantic region. The growth trend of blockings in the Northern Hemisphere was faster by 54% and in the Southern Hemisphere by 26%. The results also showed that the core of the blockings in the Northern Hemisphere corresponds to the three troughs of the Northern Hemisphere, but the core of the blockings of the Southern Hemisphere is formed at the southernmost lands of the Southern Hemisphere, i.e., at the costal zones of the Southern Hemisphere continents where the temperature difference is maximum. These regions include the Philippine Archipelago, Indonesia, and Australia in the east of the Pacific Ocean, and the coasts of Chile and Peru in the west of the Pacific Ocean.
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The data used in this article from the University of Missouri to address: http://weather.missouri.edu/gcc/ received. Also, the HGT data of the 500 level from the NOAA site was received to the https://psl.noaa.gov/data/gridded/data.ncep.reanalysis.pressure.html address.
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Toulabi Nejad, M., Hejazizadeh, Z., Lupo, A.R. et al. Spatio-temporal distribution of atmospheric blocking events in the Northern and Southern Hemispheres. Theor Appl Climatol 150, 491–505 (2022). https://doi.org/10.1007/s00704-022-04175-5
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DOI: https://doi.org/10.1007/s00704-022-04175-5