PDF-Climate Ocean and Sea Ice Modeling Project Phillip Wol

SOMA imulating cean esoscale ctivity 2 Computation of diffusivity via LIGHT agrangian situ lobal igh performance particle racking 3 SOMA Experimental design 4 SOMA Diffusivity A Spatial structure B Resolution dependence C Scales of mixing 5 Summary. NSW25,700*VICTASSA600,000*WA10,000* CaliforniaJAANCANADAUSAAUSTRALIAGulofAlaskaChukchiSeaHawaiianIslandsAleutianIslands Phillip Island’s Short-Tailed SHEARWATERS nature park Phillip Island’s Jeanine . Gelhaus. 8. th. grade science unit. Source:. http://nsidc.org/cryosphere/seaice/characteristics/formation.html. Arctic or Antarctic. Antarctica- "land surrounded by water“. Arctic - "water surrounded by land" . Definitions. Weather:. State of the atmosphere at a particular point in time.. Look outside.. Climate:. The accumulation of “weather” (atmospheric state) over a longer time period.. Look outside for a really long time and do statistics. . and Ice Conditions In and Near the Marginal Ice Zone: . The "Marginal Ice Zone Observations and Processes EXperiment" (. MIZOPEX. ). . Goals. : .  . Assess ocean and sea ice variability during the melt season within a key Marginal Ice Zone (MIZ) region. . Sea Ice Formation. --in Antarctica, begins forming in late summer with winds from the. . continent, evaporative cooling at ocean surface reduces . . water temperature to ~-1.8 °C. --as water temperature falls, ice crystals of fresh water begin . SuperStorms. Richard . Nolthenius. , PhD. A Condensed Digest of the Paper of Hansen, Sato, . et al. . 2016, and…. and What are the Economic and Physics Constraints on our Options to Deal with Climate Change ?. (AOSS 480 // NRE 480) . Richard B. Rood. Cell: 301-526-8572. 2525 Space Research Building (North Campus). rbrood@umich.edu. http://. aoss.engin.umich.edu. /people/rbrood. Winter 2015. February . 10, . 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. (AOSS 480 // NRE 480) . Richard B. Rood. Cell: 301-526-8572. 2525 Space Research Building (North Campus). rbrood@umich.edu. http:/. /. clasp. .engin.umich.edu. /people/rbrood. Winter . 2016. February . 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. . KEY. Aquatic Science/Earth-Space Science. 1. What is one thing that ocean currents do NOT do?. Moderate climate. Transport pollutants. Form tsunamis. Influence the diversity of life in the ocean. 2. The Global Ocean Conveyor Belt is caused by differences in…. Presented By: . Bob . Grumbine. (. NWS/NCEP). Contributors: . Hendrik Tolman . 2. Operational System Attribute(s). System Name. Acronym. Areal. . Coverage. Horz. Res. Cycle . Freq. Fcst. Length (. CLIMATE CHANGE IS ONE OF THE DEFINING ISSUES OF OUR TIME It is now more certain than ever based on many lines of evidence that humans are changing Earth146s climate The atmosphere and oceans have warm ice combined. . S. . Rynders (1), . Y. . Aksenov (1), . R. . Marsh (2), . N. . Skrilis. (2), . L. . Hosekova. (3), . D. Feltham . (3), . L. . Bertino. (4), . M. . Srokosz. (1), and . T. . Williams (4).