<--- Back to Details
First PageDocument Content
Lifted condensation level / Thermodynamic diagrams / Equivalent potential temperature / Potential temperature / Tephigram / Adiabatic process / Water vapor / Equilibrium level / Dew point / Atmospheric sciences / Atmospheric thermodynamics / Meteorology
Date: 2011-11-01 05:33:31
Lifted condensation level
Thermodynamic diagrams
Equivalent potential temperature
Potential temperature
Tephigram
Adiabatic process
Water vapor
Equilibrium level
Dew point
Atmospheric sciences
Atmospheric thermodynamics
Meteorology

The Tephigram Introduction Meteorology is the study of the physical state of the atmosphere. The atmosphere is a heat engine

Add to Reading List

Source URL: www.maths.ucd.ie

Download Document from Source Website

File Size: 360,61 KB

Share Document on Facebook

Similar Documents

Worksheet: Temperature (*Use sentences.)  name: 1. *Examine the diagrams on pageThe Sun is actually much larger than Earth.) Why does our part of the world get more direct rays during the summer than we get during

Worksheet: Temperature (*Use sentences.) name: 1. *Examine the diagrams on pageThe Sun is actually much larger than Earth.) Why does our part of the world get more direct rays during the summer than we get during

DocID: 1qGOD - View Document

The Tephigram Introduction Meteorology is the study of the physical state of the atmosphere. The atmosphere is a heat engine transporting energy from the warm ground to cooler locations, both vertically and horizontally.

The Tephigram Introduction Meteorology is the study of the physical state of the atmosphere. The atmosphere is a heat engine transporting energy from the warm ground to cooler locations, both vertically and horizontally.

DocID: 1qfR3 - View Document

The Tephigram Introduction Meteorology is the study of the physical state of the atmosphere. The atmosphere is a heat engine transporting energy from the warm ground to cooler locations, both vertically and horizontally.

The Tephigram Introduction Meteorology is the study of the physical state of the atmosphere. The atmosphere is a heat engine transporting energy from the warm ground to cooler locations, both vertically and horizontally.

DocID: 1p3ui - View Document

Worksheet for Exploration 20.5: PV Diagrams and Work Ideal gas law: PV = nRT. In this animation N = nR (i.e., kB = 1). This, then, gives the ideal gas law as PV = NT. The work done during a thermodynamic process depends

Worksheet for Exploration 20.5: PV Diagrams and Work Ideal gas law: PV = nRT. In this animation N = nR (i.e., kB = 1). This, then, gives the ideal gas law as PV = NT. The work done during a thermodynamic process depends

DocID: 1fYkI - View Document

Copyright© 2004, School of Meteorology, University of Oklahoma. RevKnowledge Expectations for METR 3213 Physical Meteorology I: Thermodynamics Purpose: This document describes the principal concepts, technical s

Copyright© 2004, School of Meteorology, University of Oklahoma. RevKnowledge Expectations for METR 3213 Physical Meteorology I: Thermodynamics Purpose: This document describes the principal concepts, technical s

DocID: 1a8BT - View Document