Julius von Hann explained

Julius Ferdinand von Hann
Birth Date:23 March 1839
Birth Place:Wartberg ob der Aist near Linz
Death Place:Vienna
Nationality:Austrian
Occupation:Meteorologist
Known For:Hann function

Julius Ferdinand von Hann (23 March 1839 in Wartberg ob der Aist near Linz – 1 October 1921 in Vienna) was an Austrian meteorologist. He is seen as a father of modern meteorology.

Biography

He was educated at the gymnasium of Kremsmünster and then studied mathematics, chemistry and physics at the University of Vienna, then geology and paleontology under Eduard Suess and physical geography under Friedrich Simony. From 1865 to 1868, he was master at the Oberrealschule at Linz, and in 1865 was invited by Karl Jelinek to become the first editor of the Zeitschrift für Meteorologie. In 1877, he succeeded Jelinek as the director of the Meteorologische Zentralanstalt (Central Institute for Meteorology and Earth Magnetism) and was appointed professor of meteorology at the University of Vienna. In 1897, he retired as director and became professor of meteorology at the University of Graz, but returned to Vienna to fill the chair of professor of cosmic physics in 1900, where he remained until 1910. He became an international honorary member of the American Academy of Arts and Sciences in 1902.[1] In 1912, he was made a foreign knight of the Prussian Ordre Pour le Mérite.

Hann window

Hann invented a weighted moving average technique for combining meteorological data from neighboring regions, using the weights [1/4, 1/2, 1/4], known as Hann smoothing.[2]

In signal processing, the Hann window is a window function, called the Hann function, derived from this technique by R. B. Blackman and John Tukey in 1959.[3] Here, the use of the Hann window is called "hanning", e.g., "hanning" a signal is to apply the Hann window to it.[4]

Works

He contributed many papers to the Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften.

References

Notes and References

  1. Web site: Julius Ferdinand von Hann . American Academy of Arts and Sciences . October 2, 2022.
  2. Book: Hann, Julius von. Handbook of Climatology. 199. 1903. Macmillan. en. The figures under b are determined by taking into account the parallels 5° away on either side. Thus, for example, for latitude 60° we have ½[60+(65+55)÷2]..
  3. Blackman. R. B.. R. B. Blackman. Tukey. J. W.. J. W. Tukey. 1958. The measurement of power spectra from the point of view of communications engineering — Part I. The Bell System Technical Journal. 37. 1. 273. 10.1002/j.1538-7305.1958.tb03874.x. 0005-8580.
  4. Harris. Fredric J.. Jan 1978. On the use of Windows for Harmonic Analysis with the Discrete Fourier Transform. Proceedings of the IEEE. 66. 1. 51–83. 10.1.1.649.9880. 10.1109/PROC.1978.10837. The correct name of this window is “Hann.” The term “Hanning” is used in this report to reflect conventional usage. The derived term “Hann’d” is also widely used.. refHarris. 1978IEEEP..66...51H. 426548.
  5. Review of Handbook of Climatology by Dr. Julius Hann, trans. by Robert DeCourcy Ward. The Athenaeum. 3946. June 13, 1903. 756–757.