PPT-A Warm Spitzer Survey of Atmospheric Circulation Patterns

Image credit G Orton Heather Knutson Caltech In collaboration with N Lewis Arizona N Cowan Northwestern E Agol U Washington A Burrows Princeton D Charbonneau Harvard D Deming Maryland J Desert Harvard J Fortney Santa Cruz E Kite UC Berkeley J Langton Principia G Laughlin Santa Cruz A Showman Arizona. AP Environmental Science. Mr. Grant. Lesson . 45. Objectives:. Define . the terms . weather. and . climate. .. Describe . the composition, structure, and function of Earth’s atmosphere.. Relate . weather and climate to atmospheric conditions.. 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.. Lu J, L Sun, Y Wu, and G Chen. 2014. “The Role of Subtropical Irreversible PV Mixing in the Zonal Mean Circulation Response to Global Warming-Like Thermal Forcing.” . Journal of Climate, . early online. DOI:10.1175/JCLI-D-13-00372.1.. in a nutshell. Hot air rises (rains a lot) in the . tropics. Air cools and sinks in the . subtropics. (deserts). Poleward-flow is deflected by the Coriolis force into westerly jet streams in the . temperate. Spectrophotometric. Database. Patrick Ogle, Lee . Armus. , Bob . Narron. ,. Carl . Grillmair. , Justin Howell, IRS IST. Integrating Spitzer IRS Archival data into IRSA and NED. Tap into the power of IPAC database search tools. Dr. John Krasting. NOAA/GFDL – Princeton, NJ. John.Krasting@noaa.gov. Rutgers Physical Climatology. October 18, 2012. Why is there circulation to begin with?. The Earth has to maintain its radiative balance!. and Climate (Chap 6). Atmospheric General Circulation. Also: Global or planetary circulation. . The general circulation (GC) of the atmosphere is the totality of motions that characterize the . large scale. Circulation. Wind. Cyclones and Anticyclones. Sea breezes and Land Breezes. Air Masses. Fronts. Global Circulation and Climate. California Science Project. I. . Winds. There are several factors that affect the motion of air at the Earth’s surface, including:. Mr. Ross Brown. Brooklyn School for Law and Technology. How do we understand the weather?. 4 January 2015. Do now: Take out your Reference Tables.. What is the . dewpoint. when the dry-bulb temperature is 24°C and the wet-bulb temperature is 15°C. AOS 101 Weather and Climate. Lisha. M. . Roubert. University of Wisconsin-Madison. Department of Atmospheric & Oceanic Sciences. Today’s Lab. Today we will be using the tank lab to simulate the general circulation of the atmosphere. . THE PULMONARY AND SYSTEMIC CIRCULATION. .. THE PULMONARY CIRCULATION. CARRIES BLOOD BETWEEN THE HEART AND THE LUNGS.  THIS CIRCULATION BEGINS AT THE RIGHT VENTRICLE AND ENDS AT THE LEFT ATRIUM. 3. Oxygen-Poor blood is pumped out of the Right Ventricle of the Heart into the Lungs through the Pulmonary Arteries.  These are the only Arteries in the Body to Carry Deoxygenated Blood. . Atmosphere II. Current Weather. Finish Idealized Global Circulation Model. Zonal and Meridional Flow. Blocking Patterns.  . Extratropical Cyclones. For Next Class: . Review for exam and bring questions!. Can you SUGGEST reasons why the climates of these 2 places are so different?. Dalwhinnie. , Scotland, 351m . asl. Reading, England, 52m . asl. 56.9. °N. 51.45. °N. Global Atmospheric and Oceanic Circulation. in CMIP5 GCM projections. . for the British . Isles. -. (. winters. 20. 09. –2. 099. ). Jan Stryhal & Radan Huth. Faculty . of Science, Charles University, Prague. Institute of Atmospheric Physics, Academy of Sciences of the Czech Republic, Prague .