'Radiation budget' presentation slideshows

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Atmospheric and Oceanic Aerosols and Climate

College of Marine Studies. Coast Day. October 4, 1998. Atmospheric and Oceanic Aerosols and Climate. Magdalena Anguelova Ph.D. Student Advisor: Prof. Ferris Webster. Duration: 45 min. A sunrise over the China Sea. This photograph

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METR 125 Physical Meteorology: Radiation and Cloud Physics

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Operational Climate Monitoring from Space The Satellite Application Facility on

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Can we measure from satellites the cloud effects on the atmospheric radiation budget?

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Proposal for a new IRC working group on the Global Energy Balance

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Heat Transfer and the Natural Greenhouse Effect

Heat Transfer and the Natural Greenhouse Effect. Lesson 2. Trapping Heat. Greenhouses allow us to grow plants that normally start much later in the year or require much warmer climates. Sunlight passes through the glass in the windows of the greenhouse.

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History of Space Satellites 1957- 2004

History of Space Satellites 1957- 2004. By Matt Robertson. Satellites. Satellites can be found all over the outside of the atmosphere above Earth. They allow us to have television channels, cell phones, radio stations, and much more. Today we will learn. Overview of satellites

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The World Radiation Monitoring Center and the Baseline Surface Radiation Network

The World Radiation Monitoring Center and the Baseline Surface Radiation Network. Do we Understand Climate Change?. What Makes our Climate?. The Radiation Budget. The Local Radiation Budget can be measured. Example:. 13. 1365. The Main Objectives of the

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The WMO/GAW Integrated Global Aerosol Observing and Analysis System

The WMO/GAW Integrated Global Aerosol Observing and Analysis System. John A. Ogren Earth System Research Laboratory National Oceanic and Atmospheric Administration Boulder, CO, USA (with a lot of help from Len Barrie and Urs Baltensperger). OBJECTIVE.

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Thermal Radiation Down-welling Long-wave Fluxes at the Surface

Thermal Radiation Down-welling Long-wave Fluxes at the Surface. Isabel F. Trigo. MSG-based Radiation Products Down-welling Long-wave Flux (DSLF) Definition Algorithm Basis The LSA SAF DSLF product from MSG Validation. Solar Radiation. Thermal Radiation. 30%. 23%. 90%. 4%. 47%.

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The CM-SAF expections on EURO4M

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INTRODUCTION

Cloud and water vapour variability: models, reanalyses and observations Richard P. Allan and Tony Slingo Environmental Systems Science Centre, University of Reading. INTRODUCTION. Hydrological cycle and climate feedbacks What determines the trends and variability of water cycle?

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MND Bringing Data from NASA Satellites to Your Classroom

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Cirrus Production by a Mesoscale Convective System Sampled During TWP-ICE: Analysis via Water Budget Equations

Cirrus Production by a Mesoscale Convective System Sampled During TWP-ICE: Analysis via Water Budget Equations. C su. E sd. LW. SW. *. ANVIL. CONV. STRATIFORM. MIXED ANVIL. ICE ANVIL. *. *. E se. *. *. *. A c. (D Z A ) I. A s. *. *. C T. E ce. *. *. (D Z A ) M. *. LW.

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