Pressure gradient - PDFSEARCH.IO - Document Search Engine

Pressure gradient
Results: 65

#	Item
31	TechnicAl ReAdout Acoustical operating principal: Pressure gradient or pure pressure (depending on capsule) Sensitivity (1kHz into 2.5kΩ): 27mV/Pa (+/−10mV depending on capsule) Add to Reading List Source URL: cdn.bluemic.com Language: English Signal processing Blue Microphones Sound Audio engineering Phantom power Re-amp Microphones Sound recording Electronics
32	EOS 340 Assignment 4 Due date: March 09, [removed]Extreme Surface Winds Over The Ocean Read the article, “Mapping High Sea Winds From Space” by T. Sampe and S.-P. Xie, in the December 2007 issue of Bulletin of the Ame Add to Reading List Source URL: web.uvic.ca Language: English - Date: 2012-02-21 12:53:44 Fluid dynamics Geostrophic wind Wind Geostrophic current Pressure gradient Centripetal force Geopotential height High-pressure area Pressure-gradient force Meteorology Atmospheric sciences Atmospheric dynamics
33	INSTITUTE OF PHYSICS PUBLISHING BIOINSPIRATION & BIOMIMETICS doi:[removed]/1/2/R01 Add to Reading List Source URL: www.mor-fin.com Language: English - Date: 2012-05-08 22:14:01 Aerospace engineering Dynamics Drag Dolphin Parasitic drag Reynolds number Boundary layer Flow separation Adverse pressure gradient Aerodynamics Fluid mechanics Fluid dynamics
34	QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY Q. J. R. Meteorol. Soc. 135: 1321–[removed]Published online 10 June 2009 in Wiley InterScience (www.interscience.wiley.com) DOI: [removed]qj.428 Tropical cyclone Add to Reading List Source URL: met.nps.edu Language: English - Date: 2011-10-21 13:47:13 Aerodynamics Atmospheric dynamics Vortices Vortex Balanced flow Coriolis effect Adverse pressure gradient Planetary boundary layer Boundary layer Meteorology Atmospheric sciences Fluid dynamics
35	Secondary Adaptation of Tetrapods to Life in Water, J.-M. hlazin & V. de Buffrenil (eds.): pp[removed], 14 figs[removed]by Verlag Dr. Friedrich Pfeil, Munchen, Germany - ISBN[removed]A mechanism for evolutionary tra Add to Reading List Source URL: darwin.wcupa.edu Language: English - Date: 2014-10-29 09:35:15 Fluid dynamics Dynamics Locomotion Aquatic locomotion Drag Fin Parasitic drag Adverse pressure gradient Airfoil Aerodynamics Aerospace engineering Fluid mechanics
36	Cell Permeability Changes in the extracellular osmotic pressure will create a situation in which a cell will attempt to attain equilibrium by either gaining or losing water until there is no osmotic gradient across the p Add to Reading List Source URL: people.ucalgary.ca Language: English - Date: 1999-10-20 15:20:05 Cell membrane Lipid bilayer Semipermeable membrane Aquaporin Osmotic pressure Biological membrane Red blood cell Tonicity Membrane transport Biology Membrane biology Osmosis
37	Pressure and Temperature structure of the atmosphere: • Pressure gradient controlled by ‘hydrostatic equilibrium’ — pressure supports weight of gas above it, and, because it is gas, density drops with decreasing Add to Reading List Source URL: web.gps.caltech.edu Language: English - Date: 2014-12-10 12:58:09 Atmospheric dynamics Atmosphere Tropical meteorology Intertropical Convergence Zone Low-pressure area Coriolis effect Atmosphere of Earth Troposphere Benoît Paul Émile Clapeyron Atmospheric sciences Meteorology Atmospheric thermodynamics
38	Atmos. Chem. Phys., 14, 13471–13481, 2014 www.atmos-chem-phys.net[removed]doi:[removed]acp[removed] © Author(s[removed]CC Attribution 3.0 License. Dynamical analysis of sea-breeze hodograph rotation in Sard Add to Reading List Source URL: www.atmos-chem-phys.net Language: English - Date: 2014-12-18 03:14:38 Wind Coriolis effect Low-pressure area High-pressure area Cyclone Pressure gradient Anticyclone Pressure-gradient force Meteorology Atmospheric sciences Atmospheric dynamics
39	Winter Weather Basics: Cold Air Outbreaks Or…”Exactly why is it so cold out there?” 2014 Winter Talk Series National Weather Service Gaylord, MI Add to Reading List Source URL: www.crh.noaa.gov Language: English - Date: 2014-11-26 11:03:57 Jet stream Low-pressure area High-pressure area Weather front Trough Wind Temperature gradient Weather Air mass Atmospheric sciences Meteorology Atmospheric dynamics
40	ATMO 200 – Atmospheric Processes and Phenomena Professor: Gary M. Barnes, HIG 335, [removed], ([removed]Office Hours: anytime except when other classes occur (W 3:15 to 4:30; T, TH 10:30 – 11:45) Add to Reading List Source URL: www.soest.hawaii.edu Language: English - Date: 2014-08-20 20:35:22 Oceanography Pressure gradient Low-pressure area High-pressure area Synoptic scale meteorology Weather front Weather Climate Meteorology Atmospheric sciences Atmospheric dynamics

UPDATE