## Tananyag fejlesztés idegen nyelven

Tananyag fejlesztés idegen nyelven. Prevention of the atmosphere KÖRNYEZETGAZDÁLKODÁSI AGRÁRMÉRNÖKI MSC (MSc IN AGRO-ENVIRONMENTAL STUDIES). Fundamentals to global warming (radiative forcing, feedback factor, GWP, LOSU). Lecture 9 Lessons 25-27. Lesson 25

By ostinmannual
(392 views)

## AS Geography

AS Geography. Atmosphere & Weather Energy Budgets. Meteorology is the study of the atmosphere. Weather is the short term conditions of the atmosphere. Climate is the longer-term average conditions in the atmosphere (temperature, humidity, precipitation). Structure of the atmosphere.

By tobias
(147 views)

## http://www.astro.virginia.edu/class/skrutskie/astr121/notes/

Energy Balance: Light and Heat. http://www.astro.virginia.edu/class/skrutskie/astr121/notes/. Light meter. Secchi disk. Kalff 2002. Energy Balance: Light and Heat. PAR: Photosynthetically-available radiation [radiation usable in photosynthesis]. Guildford et al. 2000.

By avalon
(135 views)

## Patterns in environmental quality and sustainability

Patterns in environmental quality and sustainability. The syllabus says: Atmosphere and change

By paiva
(80 views)

## Comparing Sources of Damping of cross-wind Motion

Comparing Sources of Damping of cross-wind Motion. Niels Jacob Tarp-Johansen, DONG Energy Christian Mørch, DONG Energy Lars Andersen, AUU Erik D. Christensen, DHI Sten Frandsen, Risø/DTU Bjarne Kallesøe, Risø/DTU Danish R&D project: HAVDIM Coordinator Risø/DTU. Outline.

By lesa
(165 views)

## Estimating ET Type of method used will be determined by:

Estimating ET Type of method used will be determined by: 1. Type of surface (e.g. open water vs. leaf) 2. Availability of water for evaporation 3. 4. 5. Amount of air-advected energy Free-water and lake evaporation - start with simplest situation, evaporation from an open water body

By mauve
(143 views)

## Chapter 6: Global Fluxes and The Deep Circulation Heat Budget Conservation of Salt

Chapter 6: Global Fluxes and The Deep Circulation Heat Budget Conservation of Salt Oceanic Water Masses Oceanic Mixing Temperature - Salinity Diagrams. NOTES. The temperature and salinity of water in the ocean are determined while that water is at the surface .

By chars
(149 views)

## Earth’s Atmosphere

Earth’s Atmosphere. Blue Planet Lab 102L Fall 2010. Image from http://www.fs.fed.us/rm. nitrogen (N 2 ) oxygen (O 2 ) argon (Ar) trace gases. Atmospheric Composition. major gases. trace gases. from Wikimedia commons. Greenhouse Gases. water (H 2 O) carbon dioxide (CO 2 ) 0.035%

By yovela
(114 views)

## The Atmospheric Layers

The Atmospheric Layers. Work. Radiation. Latent Heat. Evaporation. VAPOR. WATER. Condensation. Pressure and volume variation. Sensible Heat. T in > T out. T in < T out. The Gas Energy Exchanges. Incoming and Emitted Radiation. Incoming Solar Radiation. -2. 100%. -. 343 Wm.

By luigi
(143 views)

## Tananyag fejlesztés idegen nyelven

Tananyag fejlesztés idegen nyelven. Prevention of the atmosphere KÖRNYEZETGAZDÁLKODÁSI AGRÁRMÉRNÖKI MSC (MSc IN AGRO-ENVIRONMENTAL STUDIES). Fundamentals to global warming (radiative forcing, feedback factor, GWP, LOSU). Lecture 9 Lessons 25-27. Lesson 25

By honora
(138 views)

## Fraction of maximum leaf conductance as a function of environmental variables

Fraction of maximum leaf conductance as a function of environmental variables. C leaf = C* leaf • f K (Kin) • f  (   v ) • f T (Ta) • f  (   v ). If all functions =1, then leaf conductance and ET are maximized for the environmental conditions. If f  (   v ) = 1

By morna
(62 views)

## Modeling a Microclimate within Vegetation

Modeling a Microclimate within Vegetation. Hisashi Hiraoka Academic Center for Computing and Media Studies Kyoto University. NATO ASI, KIEV 2004. 1. Outline. ◊ introduction • background • review • objective ◊ explanation of our microclimate model ◊ validation of the model

By maxine
(146 views)

## Distinct properties of snow

Distinct properties of snow. High reflectivity or albedo Low thermal conductivity & heat capacity Limited by 0 o C (low energy status) Reservoir for water & heat Porous and translucent Mobile & smooth surface Varies greatly in space & time. Source: Oke (1987).

By irene-miles
(69 views)

## Design, Construction, and Simulation of a Solar Fish Dryer

The use of solar thermal systems in the agricultural sector to conserve vegetables, fruits, coffee, fish and other crops has proved to be practical, and economical feasible. Solar heating system to dry fish, food and other crops can improve the quality of the product, reducing wastage of food as a result of lack of proper preservation. Fish is traditional dry in Nigeria via smoking which is unhygienic. The traditional method of using wood fuel has negative impact on our eco system. In this research work, design, construction and optimization of a solar fish dryer were carried out. The temperature of the inner surface of the glass dryer was determined as 94.8\u00c2\u00b0C. The result obtained from the design of the drying chamber shown that an area of 0.12m2 is required for the system. Moreover, the area of the flat plate collector was obtained as 0.49m2. The temperature of the sun acting on the outer surface of the plane glass was obtained as 268.4\u00c2\u00b0C while the effective heat gain is obtained as 0.115kw. Sule Salisu | Oyejide Oluwayomi Joel | Akusu Onomine Murray \"Design, Construction, and Simulation of a Solar Fish Dryer\" Published in International Journal of Trend in Scientific Research and Development (ijtsrd), ISSN: 2456-6470, Volume-3 | Issue-2 , February 2019, URL: https:\/\/www.ijtsrd.com\/papers\/ijtsrd20299.pdf Paper URL: https:\/\/www.ijtsrd.com\/engineering\/mechanical-engineering\/20299\/design-construction-and-simulation-of-a-solar-fish-dryer\/sule-salisu\n

By teamijtsrd7123
(0 views)

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