PPT-Wind-forced dynamics of the Arctic Ocean

Andrey Proshutinsky Physical Oceanography Department AOMIP young scientists school Tuesday October 20 2009 1 Major themes Wind blows ice goes synoptic scales of variability Seasonal changes and effects. Rockefeller Jr Memorial PKWY Big Hole NB Cowpens NB Fort Donelson NB Fort Necessity NB Moores Creek NB Petersburg NB Stones River NB Tupelo NB Wilsons Creek NB Kennesaw Mountain NBP Richmond NBP Brices Cross Roads NBS Chickamauga and Chattanooga NMP Presentation by Kathleen Crane. Arctic Research, Climate Program Office. National Oceanic and Atmospheric. Administration. kathy.crane@noaa.gov. NOAA’s Role in the Arctic:. Ocean Observations. Atmospheric . Susan Howard. Earth & Space Research. Basically – why and how the ocean and atmosphere MOVE!. www.ametsoc.org . There are many scales of motion: . From . BIG. . to . very small. Today – I will just cover the basic large scale, GLOBAL circulation.. Dan Whitt. dw494@cam.ac.uk. D. B. Whitt and L. N. Thomas, 2015: Resonant Generation and Energetics of Wind-Forced Near-Inertial Motions in a Geostrophic Flow. . J. Phys. . Oceanogr. .. , 45, 181–208.. Equatorial ocean. A short course on:. Modeling IO processes and phenomena . INCOIS. Hyderabad, India. November 16−27, 2015. References. 1) (HIG . Notes). . McCreary, J.P., 1980: Modeling wind-driven ocean circulation. JIMAR 80-0029, HIG 80-3, Univ. of Hawaii, Honolulu, 64 pp. O. bservatory . for the . S. tudy of . A. rct. i. c . C. limate. Ad hoc Organizing Committee. Matthew Shupe – U. of Colorado. Klaus . Dethloff. – Alfred Wegener Inst. .. Ola . Persson. – U. of Colorado. The vanishing veneer of frozen ocean isn't just important for polar bears.. By: Russell . McLendon. 11/6/2015. 2. The Arctic hasn't been itself lately. Temperatures there are rising at twice the global rate, sparking an array of changes unlike anything in recorded history. One of the most striking examples is the region's sea ice, whose dramatic decline over the past decade has led to forecasts of an ice-free Arctic Ocean as early as the 2030s. . Presented To: . 7. th. Ice Diminished Arctic Symposium. RADM David J. Hahn. Chief of Naval Research . Office of Naval Research. 18 July 2017. Distribution Statement A: Approved for public release. MAJOR THRUSTS:. . . resol. . of 0.44°. (ca. 50 km x 50 km). 13 Participating. Institutes . (alphabetically). . which. . run. . circum-Arctic. RCMs. AWI. Potsdam, Germany. CCCma. Victoria, Canada. Colorado. . - 2 - some few districts beavers and martens are still scarce in many others they have increased to the extent that no harm will result in allowing them to be killed during at least one season If afte Understand sea-ice dynamics, ecosystem processes, ecosystem services and climate feedbacks in the Beaufort and Chukchi seas and the contiguous Arctic Ocean.. Understand high-latitude terrestrial ecosystem processes, ecosystem services and climate feedbacks.. By: Sean Meisner, Amanda Onwukwe, Arrian Bolden Pd:2nd. What Is Wind?. Wind: Is air moving across the surface of the Earth. Wind occurs because sunlight heats the earth’s atmosphere and surface unevenly.. Arctic research at the University of Washington is spread across many departments, with hundreds of researchers working in fields that include cryosphere, atmosphere and ocean sciences, ecology and biological sciences, fisheries, policy, social sciences, and technology development.. Andrey Proshutinsky. 1. , Eiji Watanabe. 2. , Elena Golubeva. 3. , Christophe Herbaut. 4. , Marie-Noelle Houssais. 4. , . Jiayan. Yang. 1. , Jinlun Zhang. 5. , . Yevgeny. Aksenov. 6. and Beverly de Cuevas.