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Wednesday, August 5, 2020 | History

3 edition of Evaporation, evapotranspiration and climatic data found in the catalog.

Evaporation, evapotranspiration and climatic data

Robert D. Burman

Evaporation, evapotranspiration and climatic data

by Robert D. Burman

  • 155 Want to read
  • 12 Currently reading

Published by Elsevier in Amsterdam, New York .
Written in English

    Subjects:
  • Evapotranspiration.,
  • Evaporation (Meteorology),
  • Crops and climate.

  • Edition Notes

    Includes bibliographical references (p. 251-270) and index.

    StatementR. Burman, L.O. Pochop.
    SeriesDevelopments in atmospheric science ;, 22
    ContributionsPochop, L. O.
    Classifications
    LC ClassificationsQC915 .5.B87 1994
    The Physical Object
    Paginationxxiii, 278 p. :
    Number of Pages278
    ID Numbers
    Open LibraryOL1228546M
    ISBN 100444819401
    LC Control Number94229734
    OCLC/WorldCa31257522

    Get this from a library! Estimating Pan evaporation and evapotranspiration from climatic data. [Jerald Emmet Christiansen; Utah State University. Agricultural . The book is a thorough presentation of theoretical and applied aspects of the evaporation and evapotranspiration process supported by data from experimental studies. It is written in a way that the theoretical background of evaporation and evapotranspiration estimation is presented in a simplified manner, comprehensive to most technical readers. The book deals with details of meteorological.

      The book is a thorough presentation of theoretical and applied aspects of the evaporation and evapotranspiration process supported by data from experimental studies. It is written in a way that the theoretical background of evaporation and evapotranspiration estimation is presented in a simplified manner, comprehensive to most technical : Springer Netherlands. 1. Take into consideration more of the climatic parameters that affect evaporation and evapotranspiration. 2. Use climatic data of the type published in the Weather Bureau's State Climatological Data. 3. eas y to apply. The approach was both rational and empiricaL The bas ic formula can be written. 9.

    The evapotranspiration (ET) is the amount of water transferred to the atmosphere by evaporation from the soil and plant transpiration: Evapotranspiration = Evaporation + transpiration. Evaporation and Climate. In order to understand why growing food uses so much water, we need to explore the process of evaporation. Evaporation is a hydrologic process that we're all quite familiar with, even if you aren't aware of it. Think about hanging clothes out to .


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Evaporation, evapotranspiration and climatic data by Robert D. Burman Download PDF EPUB FB2

The book is a thorough presentation of theoretical and applied aspects of the evaporation and evapotranspiration process supported by data from experimental studies. It is written in a way that the theoretical background of evaporation and evapotranspiration estimation is presented in a simplified manner, comprehensive to most technical by: The problem of estimating evaporation from water surfaces and evapotranspiration (ET) via plants is addressed in this volume.

The use of climatic data is stressed. Recent developments that are covered involve both direct estimation of evapotranspiration and the use of an intermediate step of calculating reference crop evapotranspiration. Evaporation, evapotranspiration and climatic data book Robert D Burman, L.

O Pochop Published in in Amsterdam New York by ElsevierCited by: This text addresses the problems of estimating evaporation from water surfaces and evapotranspiration (ET) via plants.

The use of climatic data is stressed. Topics discussed include soil nomenclature and parameters, and algorithms that reduce ET because of low soil moisture conditions. Book Review: Evaporation, evapotranspiration and climatic data.

Burman and L.O. Pochop, Elsevier, Amsterdam, The Netherlands, Hardcover, xxiii + pp., $Cited by: 1. The book is a thorough presentation evapotranspiration and climatic data book theoretical and applied aspects of the evaporation and evapotranspiration process supported by data from experimental Evaporation.

It is written in a way that the theoretical background of evaporation and evapotranspiration estimation is presented in a simplified manner, comprehensive to most technical readers. Pan Evaporation and Evapotranspiration from Climatic Data.

Pan evaporation data are useful in estimating losses from reservoirs and lakes, and for estimating evapotranspiration from agricultural crops using procedures relating evapotranspiration to pan evaporation.

A formula, developed at Utah State University, is presented for estimating pan evaporation from extraterrestrial radiation and climatic by: This report details the evaporation and evapotranspiration estimates provided by SILO.

Evaporation and evapotranspiration are affected by a wide variety of environmental and climatic effects. Users are urged to carefully consider the attributes of each evaporation (or evapotranspiration) variable to ensure the data chosen are fit for purpose.

The book is a thorough presentation of theoretical and applied aspects of the evaporation and evapotranspiration process supported by data from experimental studies.

EVAPORATION, TRANSPIRATION & EVAPOTRANSPIRATION BSF 3. Evaporation is the process during which a liquid changes into gas. Water changes to vapour through the absorption of heat One of the fundamental component of hydrological cycle Essential requirements in the process are 1.

The source of energy to vaporize the liquid water (solar or wind) 2. This book covers topics on the basic models, assessments, and techniques to calculate evapotranspiration (ET) for practical applications in agriculture, forestry, and urban science.

This simple and thorough guide provides the information and techniques necessary to develop, manage, interpret, and apply evapotranspiration ET data to practical applicCited by: 6. Temporal variations in reference evapotranspiration (ET 0) and aridity index (AI) were comprehensively investigated for 23 meteorological stations during – in the northwest quantitative contributions of the major meteorological variables to the ET 0 and AI trends were evaluated and the possible causes were also investigated.

The results showed that in the past 50 years Cited by: Mahfouf, J. Noilhan, J. Comparative study of various formulations of evaporation from bare soil using in situ data Journal of Applied Meteorology 30 Malek, E.

Microclimate of a desert playa: evaluation of annual radiation, energy, and water budgets components International Journal of Climatology 23 Distinctions are made (Figure 4) between reference crop evapotranspiration (ET o), crop evapotranspiration under standard conditions (ET c) and crop evapotranspiration under non-standard conditions (ET c adj).ET o is a climatic parameter expressing the evaporation power of the atmosphere.

ET c refers to the evapotranspiration from excellently managed, large, well-watered fields that. Monthly Climatic Data for the World (MCDW) publications contain monthly mean temperature, pressure, precipitation, vapor pressure, and hours of sunshine for approximately 2, surface data collection stations worldwide and monthly mean upper air temperatures, dew point depressions, and wind velocities for approximately observing sites.

Evaporation, Evapotranspiration, and Irrigation Water Requirements is a comprehensive reference to estimating the water quantities needed for irrigation of crops based upon the physics of evaporation and evapotranspiration (ET).

This new edition of which updates and expands the original, provides improved and standardized methods. The change in state from solid or liquid form to gaseous water vapor comprises the process of evaporation and sublimation. Evaporation occurs when input of energy onto an evaporating surface causes water molecules to pass from that surface to the atmosphere; this will occur when the vapor pressure of the air is below its saturation value.

A new technology, remote sensing application to evaporation and evapotranspiration estimation, is presented. The latest interest in the subject, climate change and evapotranspiration is presented in the last chapter.

This book will be beneficial to students, hydrologists, engineers, meteorologists, water managers and others. SEES Sustainable Water Resources 2/30 4.

EVAPORATION AND EVAPOTRANSPIRATION Introduction Evaporation: The process through which water is transferred from the surface of the Earth to the atmosphere.

Evaporation is important in all areas of water resources Because it affects the capacity of the reservoir, the yield of river basin, the consumptive use of water by plants.

etc. Evapotranspiration (ET) is a term used to describe the sum of evaporation and plant transpiration from the Earth's land surface to atmosphere. Evaporation accounts for the movement of water to the air from sources such as the soil, canopy interception, and water bodies.

Evapotranspiration is an important process in the water cycle because it is responsible for 15% of the atmosphere’s water vapor. Without that input of water vapor, clouds couldn’t form and precipitation would never fall. Evapotranspiration is the combined name for the processes of evaporation .A useful equation for evaporation rate E is: E = P sat (1-h)(a+bv) EQ 1.

where P sat is the vapor pressure of saturated air at the temperature of the water, v is the wind speed, and a and b are constants. Measurements and Data. Evapotranspiration Measurement.IDCKWCDE5 Prepared at GMT on Tuesday 26 May More information.

If you are using these pages, you are deemed to have understood the important information in these cover how the data are obtained, how they are processed, and what each column means.