'Free atmosphere' presentation slideshows

Astronomical site evaluation at Dome Fuji on the Antarctic plateau

Astronomical site evaluation at Dome Fuji on the Antarctic plateau. Hirofumi OKITA. June 17, 2013. Based on Okita et al., A&A, 554, L5 (2013) and some unpublished results. Contents. Introduction Instrumentations Data processing and error analysis Results Discussion and conclusion

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Operational and Research Activities at ECMWF

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Inhibiting Microbial Growth in vitro

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A multiline LTE inversion using PCA

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17th International ABP Induction Conference 2013

516 views • 33 slides

Deep Convection: Initiation

Deep Convection: Initiation. Deep Convection: Initiation. Convective Initiation Big Picture Boundary Layer Basics Boundary Layer Convection Initiation on the Mesoscale. Deep Convection: Initiation. Convective Initiation: Where and when will moist convection develop?

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Polarized and Fluorescence Microscope (PFLM)

Polarized and Fluorescence Microscope (PFLM). Leica Microsystems, ( Wetzlar , Germany). The PFLM comes with a digital camera and 46 components including specialty filters, eyepieces and light source. This instrument is equipped with a temperature controlled stage (Linkam LTS 350).

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Models of the ground layer and free atmosphere at some sites

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Chen Deng-Shun 16 Apr, 2013, NCU

Determining Key Model Parameters of Rapidly Intensifying Hurricane Guillermo(1997) Using the Ensemble Kalman Filter . Chen Deng-Shun 16 Apr, 2013, NCU .

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Temperature

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The simplifed momentum equations

The simplifed momentum equations. Height coordinates. Pressure coordinates. In this section we will examine the effect of friction on the wind in the boundary layer.

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Thermally-Driven Circulations

Thermally-Driven Circulations. What two countries were the Apollo astronauts viewing? Do you see any intriguing cloud formations?. Thermally-Driven Circulations. Land-Sea Breezes Slope-Valley Flows Urban Heat Island Circulations. Land-Sea Breeze. Definition:

370 views • 21 slides

CREPC Going Forward

CREPC Going Forward. April 15, 2010 South Congregational Church Hartford, CT Conducted for CREPC Leadership by: Carmine Centrella, CRCOG Homeland Security Planner Daniel Scace, CRCOG Regional Training Coordinator Hartford Area UASI Program Manager. Purpose.

394 views • 20 slides

Observed Structure of the Atmospheric Boundary Layer

Observed Structure of the Atmospheric Boundary Layer. Many thanks to: Nolan Atkins, Chris Bretherton, Robin Hogan. Review of last lecture: Surface water balance. The changing rate of soil moisture S dS/dt = P - E - Rs - Rg + I. Precipitation (P). Evaportranspiration (E=Eb+Ei+Es+TR).

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DIAMONDS

DIAMONDS. INDEX. Mining and places of mining. Types of diamond. Why hardest? Chemical Properties. Cutting and polishing. Instruments. 5 Famous Diamonds Companies. Mining and places of mining. Diamond Mining Diamonds are recovered by way of pipe or alluvial mining.

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Changes in the Free Atmosphere

Changes in the Free Atmosphere. Current Weather Data Sources Weather Balloons Tropospheric and Stratospheric Temperatures Tropopause Height For Next Class: Read IPCC AR4 Ch. 3 (pp. 280-295). Data Sources for Analyzing Tropospheric Temperature Trends. Radiosondes

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The Atmospheric Boundary Layer (ABL) over Mesoscale Surface Heterogeneity

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Boundary Layer Physics 14 May 2007

Boundary Layer Physics 14 May 2007. Claudia.Kubatzki@awi.de Literature: R.B. Stull (1988, new edition 1999): An Introduction into Boundary Layer Meteorology . Kluwer Academic Publishers, Dordrecht, Netherlands. Atmospheric Layers. z [m]. ~10 4. Free Atmosphere. ~10 3. Ekman Layer.

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Introduction

Introduction. In this tutorial, you will learn that there are two types of memorization and you will be given some suggestions on how to memorize better in both types. . Which type you need.

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The GCOS Reference Upper Air Network

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