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  1. Richard Siegmund Lindzen (* 8. Februar 1940 in Webster, Massachusetts) ist ein US-amerikanischer Atmosphärenphysiker und Klimaskeptiker. Von 1983 bis zu seiner Emeritierung 2013 war er Professor für Meteorologie in der Abteilung für Erd-, Atmosphären- und Planetenwissenschaft am Massachusetts Institute of Technology (MIT). Zuvor ...

  2. Richard Siegmund Lindzen (born February 8, 1940) is an American atmospheric physicist known for his work in the dynamics of the middle atmosphere, atmospheric tides, and ozone photochemistry. He is the author of more than 200 scientific papers. From 1972 to 1982, he served as the Gordon McKay Professor of Dynamic Meteorology at

    • American
  3. 13. März 2023 · 735. 21K views 1 year ago. In this video, Dr. Richard Lindzen, Ph.D., a renowned atmospheric physicist and professor emeritus at MIT, delivers a speech at the Fifteenth International Conference...

    • 24 Min.
    • 21,4K
    • The Heartland Institute
  4. 2. Mai 2024 · Richard Lindzen, Ph.D. is Alfred P. Sloan Professor of Meteorology, Department of Earth, Atmospheric and Planetary Sciences at MIT. He has made major contributions to the development of the current theory for the Hadley Circulation, which dominates the atmospheric transport of heat and momentum from the tropics to higher latitudes ...

  5. S Chapman, RS Lindzen. Springer Science & Business Media. , 2012. 1799 *. 2012. On the role of sea surface temperature gradients in forcing low-level winds and convergence in the tropics. RS Lindzen, S Nigam. Journal of Atmospheric Sciences 44 (17), 2418-2436. , 1987.

  6. 22. Sept. 2022 · Richard Lindzen, Ph.D. is Alfred P. Sloan Professor of Meteorology, Department of Earth, Atmospheric and Planetary Sciences at MIT.He has made major contribu...

    • 50 Min.
    • 18,3K
    • Tom Nelson
  7. 9. Juli 2022 · Richard S. Lindzen, a distinguished atmospheric physicist, reviews the scientific uncertainties about the impact of carbon dioxide emissions on temperature and climate sensitivity. He challenges the IPCC's assumptions and models, and highlights the role of clouds and feedbacks in the climate system.