Starting from the ground, geology; his interest surfaced the sky ending him discovering Stratosphere & Troposphere; founding aerology!!!
Posted January 2nd, 2015
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Léon Philippe Teisserenc de Bort (November 5, 1855 in Paris, France – January 2, 1913 in Cannes, France) was a French meteorologist and a pioneer in the field of aerology. Together with Richard Assmann (1845-1918), he is credited as co-discoverer of the stratosphere, as both men announced their discovery during the same time period in 1902. Teisserenc de Bort pioneered the use of unmanned instrumented balloons and was the first to identify the region in the atmosphere around 8-17 kilometers of height where the lapse rate reaches zero, known today as the tropopause.
He was the son of an engineer. He began his scientific career in 1880, when he entered the meteorological department of the Bureau Central Météorologique (Administrative Center of National Meteorology, a department of the French government) in Paris under E. E. N. Mascart. In 1883, 1885 and 1887 he made journeys to North Africa to study geology and terrestrial magnetism, and during this, period published some important charts of the distribution of pressure at a height of 4,000 metres. Between 1892 and 1896, Teisserenc de Bort was chief meteorologist to the Bureau.
After his resignation from the Bureau in 1896, he established a private meteorological observatory in Trappes near Versailles. There he carried out investigations on clouds and the problems of the upper air. He conducted experiments with high-flying instrumented hydrogen balloons and was one of the first people to use such devices.
In 1898, Teisserenc de Bort published an important paper in Comptes Rendus detailing his researches by means of balloons into the constitution of the atmosphere. He noticed that while the air temperature decreased steadily up to approximately 11 kilometers of height, it remained constant above that altitude (up to the highest points he could reach). In other words, he discovered an indication of a temperature inversion or at least of a zero lapse rate above this altitude.
For many years he was uncertain whether he discovered a true physical phenomenon or whether his measurements suffered from a systematic bias (indeed, the first measurements did have a positive temperature bias as the instruments were liable to radiative heating by solar radiation). That is why Teisserenc de Bort carried out 200+ more balloon experiments (with a substantial part of them being held during the night to eliminate radiative heating) until 1902, when he suggested that the atmosphere was divided into two layers.
During the years that followed, he named the two layers of the atmosphere known as the "troposphere" and the "stratosphere". This naming convention has since been maintained, with (higher-altitude) layers that were subsequently discovered being given names of this sort. After Teisserenc de Bort's death in 1913, the heirs donated the observatory to the state so that the research tasks could be continued.
He also carried out investigations in Sweden and over the Zuider Zee, the Mediterranean and the tropical region of the Atlantic, and fitted out a special vessel in order to study the currents above the trade winds. He was elected a fellow of the Royal Meteorological Society in 1903, honorary member in 1909, and was awarded the Symons gold medal of the Society in 1908. He collaborated with Hugo Hildebrandsson in Les bases de la météorologie dynamique (1907).

Two craters are named after him: 1. The crater Teisserenc on the Moon. 2. The crater Teisserenc de Bort on Mars.

The troposphere is the lowest portion of Earth's atmosphere. It contains approximately 80% of the atmosphere's mass and 99% of its water vapour and aerosols. The average depth of the troposphere is approximately 17 km (11 mi) in the middle latitudes. It is deeper in the tropics, up to 20 km (12 mi), and shallower near the polar regions, approximately 7 km (4.3 mi) in winter. The lowest part of the troposphere, where friction with the Earth's surface influences air flow, is the planetary boundary layer. This layer is typically a few hundred meters to 2 km (1.2 mi) deep depending on the landform and time of day. The border between the troposphere and stratosphere, called the tropopause, is a temperature inversion.

The stratosphere is the second major layer of Earth's atmosphere, just above the troposphere, and below the mesosphere. It is stratified in temperature, with warmer layers higher up and cooler layers farther down. This is in contrast to the troposphere near the Earth's surface, which is cooler higher up and warmer farther down. The border of the troposphere and stratosphere, the tropopause, is marked by where this inversion begins, which in terms of atmospheric thermodynamics is the equilibrium level. At moderate latitudes the stratosphere is situated between about 10–13 km (33,000–43,000 ft; 6.2–8.1 mi) and 50 km (160,000 ft; 31 mi) altitude above the surface, while at the poles it starts at about 8 km (26,000 ft; 5.0 mi) altitude, and near the equator it may start at altitudes as high as 18 km (59,000 ft; 11 mi).

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