![]() Alfred Wegeners theory states that only one. The first truly detailed and comprehensive theory of continental drift was proposed in 1912 by Alfred Wegener, a German meteorologist.Bringing together a large mass of geologic and paleontological data, Wegener postulated that throughout most of geologic time there was only one continent, which he called Pangea. ![]() An integrative analysis of the annual budget of excess heat and carbon will be produced for the Atlantic sector of the Southern Ocean. It was Alfred Wegener (1880-1930) who proposed the theory of continental drift and was the first to hypothesize the drifting of continents in 1912. New and existing time series data of heat and salinity from the Weddell Sea shelf and slope regions will be collated and analysed for dense water formation and water mass modification on the shelf and export down the slope. Our contribution is to conduct new measurements of the partial pressure of CO2, couple them with existing data and analyse those for the seasonal cycle. Boebel) and WP6 on decadal variability of heat and carbon storage (T. Hoppema, WP co-leader), WP3 on deep ocean ventilation pathways (T. Role in projectĪWI contributes to three work packages, WP1 on air-sea fluxes (M. Recently for the external review of the AWIwide research program the institute became the grade “outstanding”. It also contributes to a variety of international research programmes and projects like the European Multidisciplinary Seafloor Observatory (EMSO), the Integrated Carbon Observation System (ICOS PI Hoppema being AWI representative), Partnership for Observation of the Global Oceans (POGO) and the Earth System Science Partnership (ESSP). Through memberships, the AWI is embedded in a number of European Research initiatives, such as the European Polar Board (EPB), the European Marine Board (EMB), and the European Climate Research Alliance (ECRA). Wegener was an eclectic scientist, with interests ranging from historical astronomy to aerology, the study of lunar craters, and the theory of continental drift for which he became best known. 1924-1930 (Public domain, via Wikimedia Commons). Responsibilities include biological monitoring, providing scientific-technical support for German and international polar research, and updating the German federal government on research results and giving advice for development of environmental policies.ĪWI keeps up an extensive cooperation with numerous national and international institutions. Alfred Wegener was born in Berlin in 1880, and his life in many ways tells the story of the developing earth sciences in the early 20th century. AWI has a coordinating function, offers advice and consultancy, and provides special services. ![]() This site is managed by the Directorate-General for Maritime Affairs and Fisheries (DG MARE). It has an annual budget of more than 100 million Euro. European Marine Observation and Data Network (EMODnet). AWI was established as a public foundation in 1980 and includes the headquarters in Bremerhaven, and four further research units in Germany. With a staff of more than 1000 employees, about half of them scientists at levels between graduate students and full professors, AWI conducts multidisciplinary research mainly in the Arctic and Antarctic. This slideshow explains Wegener’s theory.The AWI is a member of the Helmholtz Association of German Research Centres (HGF), the largest science organisation in Germany. It was not until the 1960s that evidence of convection currents within the mantle was discovered to support the theory fully. One of the reasons was that it was difficult to work out how whole continents could move. ![]() It took more than 50 years for Wegener’s theory to be accepted. For example, the Himalayas formed when India came into contact with Asia. Such was the fate of Alfred Wegener (1880-1930), a German scientist who lived and died with the unwavering conviction that the ground we stand upon is not as solid as it seems. Wegener suggested that mountains formed when the edge of a drifting continent collided with another, causing it to crumple and fold. Sometimes he freezes to death, on an expedition in an Arctic wasteland, decades before his peers finally recognize him as a visionary. He studied the natural sciences at the University of Berlin, receiving a doctorate in astronomy in 1904. If this was the case, then mountains would be spread evenly over the Earth’s surface. Alfred Wegener was born in Berlin on November 1, 1880. This process formed wrinkles, or mountains, on the Earth’s crust. īefore Wegener developed his theory, it was thought that mountains formed because the Earth was cooling down, and, as it cooled down, it contracted. The theory of continental drift was proposed at the beginning of the last century by German scientist Alfred Wegener. ![]()
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