Inge Lehmann: Difference between revisions

Inge Lehmann

Inge Lehmann was born and grew up in Østerbro, a part of Copenhagen. Her mother was Ida Sophie Tørsleff; her father was experimental psychologist Alfred Georg Ludvik Lehmann (1858–1921). She received her school education at a pedagogically progressive high school led by Hanna Adler, Niels Bohr's aunt.^[5][6] According to Lehmann, her father and Adler were the most significant influences on her intellectual development.

She studied mathematics at the

She was a very shy girl, and did not enjoy being in the spotlight too much. Even when she grew older, she was still very shy. She was schooled in a private school, after taking the entrance exam for Copenhagen University with the first rank mark. She started freshman courses in mathematics, chemistry and physics. It took her an exceptionally long time to get a degree: in 1911 she had returned to Copenhagen after a year at Cambridge University completely burned out; she then abandoned her studies to do actuarial work for an insurance company. She did actuarial work until 1918, when she returned to university, finally graduating with a mathematics degree in 1920, aged 32. She then started working as an assistant in Copenhagen University's actuarial department and later shifted her interest to seismology work with Professor Niels Norlund. She learned that the internal structure of our planet can be understood through the study of earthquake data. She travelled a lot of places just to get a better understanding of the earth's movement.[8]^[9][10]

Lehmann had a younger sister, Harriet, who became a movie writer and who had family and children in contrast to Lehmann, who lived by herself all her life.^[11][12][13]

Career

In 1925 Lehmann became an assistant to the geodesist Niels Erik Nørlund, who assigned her the task of setting up seismological observatories in Denmark and Greenland. Based on her studies in seismology, in 1928 she earned the magister scientiarum degree (equivalent to an MA) in geodesy and accepted a position as state geodesist and head of the department of seismology at the Geodetical Institute of Denmark led by Nørlund.^[15] Lehmann looked into improving the coordination and analysis of measurements from Europe's seismographic observatories, as well as many other scientific endeavours.^[9][16]

In a paper titled P' (1936),^[17] Lehmann was the first to interpret P wave arrivals—which inexplicably appeared in the P wave shadow of the Earth's core—as reflections from an inner core, for example from the strong 1929 Murchison earthquake.^[18] Other leading seismologists of the time, such as Beno Gutenberg, Charles Richter, and Harold Jeffreys, adopted this interpretation within two or three years, but it took until 1971 for the interpretation to be shown correct by computer calculations.^[19] Lehmann was significantly hampered in her work and maintaining international contacts during World War II and the German occupation of Denmark. She served as the Chair of the Danish Geophysical Society in 1940 and 1944 respectively.

In 1952, Lehmann was considered for a professorship in geophysics at Copenhagen University, but was not appointed. In 1953, she retired from her position at the Geodetic Institute. She moved to the US for several years and collaborated with Maurice Ewing and Frank Press on investigations of Earth's crust and upper mantle. During this work, she discovered another seismic discontinuity, which lies at depths between 190 and 250 km and was named for her, the Lehmann discontinuity. Francis Birch noted that the "Lehmann discontinuity was discovered through exacting scrutiny of seismic records by a master of a black art for which no amount of computerization is likely to be a complete substitute."^[19]

Awards and honors

Lehmann received many honors for her outstanding scientific achievements, among them the Gordon Wood Award (1960), the Emil Wiechert Medal (1964), the Gold Medal of the Danish Royal Society of Science and Letters (1965), the Tagea Brandt Rejselegat (1938 and 1967), her election as a Fellow of the Royal Society in 1969,^[20] the William Bowie Medal (1971, as the first woman), and the Medal of the Seismological Society of America in 1977. She was awarded honorary doctorates from Columbia University in 1964 and from the University of Copenhagen in 1968, as well as numerous honorific memberships.

The asteroid

Because of her contribution to geological science, in 1997, the American Geophysical Union established the annual Inge Lehmann Medal to honor "outstanding contributions to the understanding of the structure, composition, and dynamics of the Earth's mantle and core."^[9][22][23]

On the 127th anniversary of her birth, Google dedicated its worldwide Google Doodle to her.^[24][25][26]

A new memorial dedicated to Lehmann was installed on Frue Plads in Copenhagen in 2017. The monument is designed by Elisabeth Toubro.^[27]

Key publications

• Lehmann, Inge (1936). "P'". Publications du Bureau Central Séismologique International. A14 (3): 87–115.

See also

• Richard Dixon Oldham
• List of geophysicists

References