PPT-Synoptic Scale Balance Equations

Using scale analysis to identify the dominant forces at work and manipulating the equations of motion we can arrive at geostrophic balance deviations from geostrophic balance curvature and friction . Stephen Rodriguez, Jr.. National Weather Service Chicago, IL. Introduction. Brief background.. Purpose of Study.. Synoptic background and forcing mechanisms.. Synoptic/. Mesoscale. features: Moisture, Forcing, Instability.. Lesson Objective:. An equation is like a set of scales.. To keep it balanced, whatever you. do to one side you must do to the other.. Use this idea to solve equations like:. 3x + 1 = x + 7 . 2 (3x + 1) = 3 (x – 2). Outline. Time Derivatives & Vector Notation. Differential Equations of Continuity. Momentum Transfer Equations. Introduction. FLUID. In order to calculate forces exerted by a moving fluid as well as the consequent transport effects, the dynamics of flow must be described mathematically . Hands-On Algebra with Fractions and Mixed Numbers. Connecting to Algebra . When you hear the word “algebra”, what do you think of?. What are some things you know about algebra?. How might you use algebra in real-life?. I can identify the products and reactants in a chemical reaction.. I can state the law of conservation of matter.. I can determine the number of each atom in a compound based on subscripts and coefficients.. Cyclone . Structure. QG Theory. NAM Forecast Sounding for this Saturday at 03 UTC (i.e., tonight near 9pm). In the . sfc. to ~700-mb layer, how are the winds turning with height?. Counter-clockwise. Mesoscale energy sources. Gage and . Nastrom. (1985). [shifted x10 to right]. Note two spectral extremes:. (a) A maximum at about 2000 km. (b) A minimum at about 500 km. 1. 100. 10. 1000. wavelength [km]. CLINICAL PROBLEM SOLVING I. THE BERG BALANCE SCALE. AS A PREDICTOR OF disability, LEGNTH OF STAY, and DISCHARGE Destination IN POST-STROKE PATIENTS. PURPOSE. This presentation aims to describe the physical therapy examination, evaluation, plan of care, and outcomes of a patient who . Lecture . 1. AL-MUSTANSIRIYAH . UNIVERSITY . COLLEGE OF SCIENCES. ATMOSPHERIC SCIENCES DEPARTMENT .  . Dr. . Sama. Khalid Mohammed. SECOND . CLASS . 1. 2. Weather Maps. Surface maps, upper air maps, Observation times and collection, codes, surface . Lecture . 1. AL-MUSTANSIRIYAH . UNIVERSITY . COLLEGE OF SCIENCES. ATMOSPHERIC SCIENCES DEPARTMENT .  . Dr. . Sama. Khalid Mohammed. SECOND . CLASS . 1. 2. Weather Maps. Surface maps, upper air maps, Observation times and collection, codes, surface . Course Overview & Logistics. Wed – 20 Aug 2014. Introductions…. Office: NSSTC 3088. Email: . ryan.wade@uah.edu. Phone: 961-7847 (office phone). Office Hours. :. MWF: 8:00am – 9:00am, 10:15am – 11:00am. Based on EHES Manual, Part B. Fieldwork Procedures, 2. nd. edition (2016). Available at: . http://urn.fi/URN:ISBN:978-952-302-701-5. These slides . can be used freely, translated and adapted to national use (e.g. concerning the equipment). However, it is important to keep in mind that no changes should be made to the measurement techniques, which need to be standardized. . 81EquipmentStopwatch 2 lbcuff weight pen 12inch ruler slipper Physician Desk Reference 15x15x15 foamPurpose11 item ordinal scale test used to assess individuals who are primarily non ambulatory Able t Atmospheric Sciences 370. Heights and winds aloft are closely related by the geostrophic and gradient wind relationships. For 80%+ of the atmosphere outside of the inner tropics, the geostrophic relationship is quite good..