1. Complete the tables below with your measurements and determinations of the humidity variables inside and outside of the Engineering Building. In the first blank column of the table (titled Individual Measurement) fill in the boxes for the temperature and wet-bulb temperature. Average values of the temperature and wet-bulb temperature for all the measurements taken by everyone in the class will be used to complete the last column of the table (titled Average Measurement). Use the temperature and wet-bulb temperature values and the average values of these temperatures in the last column, to determine the remaining humidity variables, using the psychrometric chart. Inside the Engineering Building Humidity Variable Individual Measurement T (°C) (measured) Tw (°C) (measured) Ta (°C) Vapor Pressure: e (mb) Dew-point Depression (°C) Relative Humidity (%) Outside the Engineering Building Humidity Variable Individual Measurement T (°C) (measured) Tw (°C) (measured) Ta (°C) Vapor Pressure: e (mb) Dew-point Depression (°C) Relative Humidity (%) Answer questions 2a – 2f by considering the parameter values in the last (right-hand) column of each of the above tables. 2a. Which location has the greater relative humidity? 2b. Which location has the smaller dew point depression? 2c. How do your answers to questions 2a and 2b relate to the conclusions that you drew in lab I concerning the relationship of dew point depression and relative humidity?

Elements Of Electromagnetics
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ISBN:9780190698614
Author:Sadiku, Matthew N. O.
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ChapterMA: Math Assessment
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I need help with this lab Outside the building: Dry-bulb temp = 30oC or 86oF Wet-bulb temp = 18oC or 84oF Inside the building: Dry-bulb temp = 21oC or 70oF Wet-bulb temp = 16oC or 61oF
Lab 5 Humidity Variables
1. Complete the tables below with your measurements and determinations of the humidity variables inside and
outside of the Engineering Building. In the first blank column of the table (titled Individual Measurement) fill in the
boxes for the temperature and wet-bulb temperature. Average values of the temperature and wet-bulb temperature
for all the measurements taken by everyone in the class will be used to complete the last column of the table (titled
Average Measurement). Use the temperature and wet-bulb temperature values and the average values of these
temperatures in the last column, to determine the remaining humidity variables, using the psychrometric chart.
Inside the Engineering Building
Humidity Variable
Individual Measurement
T (°C) (measured)
Tw (°C) (measured)
Ta (°C)
Vapor Pressure: e (mb)
Dew-point Depression (°C)
Relative Humidity (%)
Outside the Engineering Building
Humidity Variable
Individual Measurement
T (°C) (measured)
Tw (°C) (measured)
Ta (°C)
Vapor Pressure: e (mb)
Dew-point Depression (°C)
Relative Humidity (%)
Answer questions 2a – 2f by considering the parameter values in the last (right-hand) column of each of the above
tables.
2a. Which location has the greater relative humidity?
2b. Which location has the smaller dew point depression?
2c. How do your answers to questions 2a and 2b relate to the conclusions that you drew in lab I concerning the
relationship of dew point depression and relative humidity?
41
Transcribed Image Text:Lab 5 Humidity Variables 1. Complete the tables below with your measurements and determinations of the humidity variables inside and outside of the Engineering Building. In the first blank column of the table (titled Individual Measurement) fill in the boxes for the temperature and wet-bulb temperature. Average values of the temperature and wet-bulb temperature for all the measurements taken by everyone in the class will be used to complete the last column of the table (titled Average Measurement). Use the temperature and wet-bulb temperature values and the average values of these temperatures in the last column, to determine the remaining humidity variables, using the psychrometric chart. Inside the Engineering Building Humidity Variable Individual Measurement T (°C) (measured) Tw (°C) (measured) Ta (°C) Vapor Pressure: e (mb) Dew-point Depression (°C) Relative Humidity (%) Outside the Engineering Building Humidity Variable Individual Measurement T (°C) (measured) Tw (°C) (measured) Ta (°C) Vapor Pressure: e (mb) Dew-point Depression (°C) Relative Humidity (%) Answer questions 2a – 2f by considering the parameter values in the last (right-hand) column of each of the above tables. 2a. Which location has the greater relative humidity? 2b. Which location has the smaller dew point depression? 2c. How do your answers to questions 2a and 2b relate to the conclusions that you drew in lab I concerning the relationship of dew point depression and relative humidity? 41
Lab 5 Humidity Variables
NAS 125 Meteorology Lab 5
Name
Humidity Variables
Main Lab Assignment
I. Introduction
Humidity is a measure of the amount of water vapor present in the atmosphere, at a given time and location.
Meteorologists use a number of different variables to represent the amount of moisture in a given sample of air. The
use of so many different variables to represent
humidity variables that will be presented in this lab has their own advantages and disadvantages.
same basic measurement may seem strange, but each of the
The humidity variables used in this lab include:
Vapor pressure
Saturation vapor pressure
Relative humidity
Dewpoint
Wet-bulb temperature
Lab Goals:
(1) Learn about humidity variables and their inter-relationships
(2) Determine relative humidity both indoors and out, using a psychrometric chart to interpret measurements
made with a sling psychrometer
II. Review of Terms
Saturation: A given sample of air (an air parcel) is said to be saturated when the rate of evaporation from a flat
surface of water into the parcel is exactly equal to the rate of water vapor condensation onto the water surface, from
the air parcel. In the atmosphere any addition of water vapor to a sample of air that is already saturated will result in
condensation and the formation of clouds or fog. Therefore, when an air parcel is referred to as "saturated," the air
contains the maximum amount of water vapor possible at the prevailing temperature, without condensation
occurring.
Vapor pressure (e): The vapor pressure is the pressure exerted by the water vapor molecules in a sample of air.
The water vapor pressure contributes to the overall pressure similarly to the pressure contributions from the other
gases present (nitrogen, oxygen, argon, etc.)
Saturation vapor pressure (e,): The saturated vapor pressure is the contribution to the total pressure from the water
vapor molecules in a sample of air that is saturated. A given air parcel will have separate values for the vapor
pressure and the saturation vapor pressure associated with it. The vapor pressure is a measure of the amount of water
vapor actually in the air parcel, while the saturation vapor pressure is a measure of the maximum amount of water
vapor the air parcel could hold at its current temperature. (Remember that the saturation vapor pressure increases as
the temperature of the air parcel increases. When the air parcel is saturated the vapor pressure will equal the
saturation vapor pressure.
Relative humidity (RH): The relative humidity is a measure of how close the air is to being saturated and is the
ratio of the actual vapor pressure to the saturation vapor pressure. (Relative humidity is also given by the ratio of the
mixing ratio to the saturation mixing ratio). Because the relative humidity is calculated based on the actual amount
of water vapor in an air parcel and the maximum amount of water vapor an air parcel could hold (which depends on
the temperature of the air parcel) the relative humidity will change if either the amount of water vapor present
changes or the temperature changes. This is an important idea to understand. It means that the relative humidity
cannot be used when comparing the actual amount of water vapor present at two different locations or times (since
the temperature may not have been the same when the two relative humidity measurements were made). If you are
interested in comparing the actual amount of water vapor present at two different locations, other humidity variables
such as the vapor pressure, dewpoint, or wet-bulb temperature must be used.
38
Transcribed Image Text:Lab 5 Humidity Variables NAS 125 Meteorology Lab 5 Name Humidity Variables Main Lab Assignment I. Introduction Humidity is a measure of the amount of water vapor present in the atmosphere, at a given time and location. Meteorologists use a number of different variables to represent the amount of moisture in a given sample of air. The use of so many different variables to represent humidity variables that will be presented in this lab has their own advantages and disadvantages. same basic measurement may seem strange, but each of the The humidity variables used in this lab include: Vapor pressure Saturation vapor pressure Relative humidity Dewpoint Wet-bulb temperature Lab Goals: (1) Learn about humidity variables and their inter-relationships (2) Determine relative humidity both indoors and out, using a psychrometric chart to interpret measurements made with a sling psychrometer II. Review of Terms Saturation: A given sample of air (an air parcel) is said to be saturated when the rate of evaporation from a flat surface of water into the parcel is exactly equal to the rate of water vapor condensation onto the water surface, from the air parcel. In the atmosphere any addition of water vapor to a sample of air that is already saturated will result in condensation and the formation of clouds or fog. Therefore, when an air parcel is referred to as "saturated," the air contains the maximum amount of water vapor possible at the prevailing temperature, without condensation occurring. Vapor pressure (e): The vapor pressure is the pressure exerted by the water vapor molecules in a sample of air. The water vapor pressure contributes to the overall pressure similarly to the pressure contributions from the other gases present (nitrogen, oxygen, argon, etc.) Saturation vapor pressure (e,): The saturated vapor pressure is the contribution to the total pressure from the water vapor molecules in a sample of air that is saturated. A given air parcel will have separate values for the vapor pressure and the saturation vapor pressure associated with it. The vapor pressure is a measure of the amount of water vapor actually in the air parcel, while the saturation vapor pressure is a measure of the maximum amount of water vapor the air parcel could hold at its current temperature. (Remember that the saturation vapor pressure increases as the temperature of the air parcel increases. When the air parcel is saturated the vapor pressure will equal the saturation vapor pressure. Relative humidity (RH): The relative humidity is a measure of how close the air is to being saturated and is the ratio of the actual vapor pressure to the saturation vapor pressure. (Relative humidity is also given by the ratio of the mixing ratio to the saturation mixing ratio). Because the relative humidity is calculated based on the actual amount of water vapor in an air parcel and the maximum amount of water vapor an air parcel could hold (which depends on the temperature of the air parcel) the relative humidity will change if either the amount of water vapor present changes or the temperature changes. This is an important idea to understand. It means that the relative humidity cannot be used when comparing the actual amount of water vapor present at two different locations or times (since the temperature may not have been the same when the two relative humidity measurements were made). If you are interested in comparing the actual amount of water vapor present at two different locations, other humidity variables such as the vapor pressure, dewpoint, or wet-bulb temperature must be used. 38
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