L.O: SWBAT to determine dewpoint and relative humidity.

Slides:



Advertisements
Similar presentations
HUMIDITY AND DEW POINT.
Advertisements

Atmospheric Humidity. Global water cycle: precipitation = evaporation.
Atmospheric Moisture. How does the moisture get in the atmosphere?? EVAPORATION TRANSPIRATION – water evaporated from trees.
RRB Pg 117.  Saturation: When the air contains as much moisture as it can hold  The higher the temperature, the more moisture air can hold  If air.
Water in the Atmosphere. Humidity Humidity is a measure of the amount of water vapor in the air. Air’s ability to hold water vapor depends on its temperature.
Saturation = filled to capacity
Topic 7. What is atmospheric moisture? Atmospheric moisture refers to the amount of water in the air All 3 phases are included: solid, liquid and gas.
How much moisture is in the air relative to how much it can hold
Moisture in the air. Heavy and Light air Heavy Air: (high pressure) – cold, because the molecules are closer together. – Dry, because nitrogen and oxygen.
1._____process that forms clouds (water cycle 2) 2._____ process that adds heat and changes liquid water to water vapor (water cycle) 3._____what powers.
What is Fog? Fog is essentially a dense cloud of water droplets, or cloud, that is close to the ground. Fog forms when warm, moist air travels over a cold.
HUMIDITY AND DEW POINT. CONDENSATION � H2O can exist in solid, liquid, or gaseous states. Change from liquid to gas is evaporation. Change from gas to.
Relative Humidity. Humidity  the measure of the amount of water in the air  high humidity =lots of moisture in the air.
Water in the Atmosphere Water vapor is the source of all condensation and precipitation. When it comes to understanding atmospheric processes, water.
Humidity Characteristics of water Humidity Condensation.
Atmospheric Moisture. How does the moisture get in the atmosphere?? EVAPORATION – liquid to a gas TRANSPIRATION – process of water being taken in and.
Aim: What is Humidity and Dew Point? Do Now: What instruments do scientist use to measure air pressure? Explain why in the daytime a breeze comes from.
1._____process that forms clouds (water cycle 2) 2.____ layer of atmosphere that weather occurs in (atm layers) 3._____ process that adds heat and changes.
Humidity The amount of water vapor in the air.. Expressed two ways Relative Humidity Dew Point.
Aim: How can we explain relative humidity and dew point?
Humidity and Dew Point. Foldable Make a two flap foldable one side Relative Humidity and the other side Dew Point Should Contain What it is How it is.
Humidity Water Vapour in the Air. The more water vapour in the atmosphere A) the air becomes heavier. B) the air becomes lighter. C) the air stays the.
Aim: What is relative humidity? Do Now: Answer the following in your notebooks; 1)What do you think of when you hear it is humid out? 2)Explain what type.
Dew Point & Relative Humidity How to use a Psychrometer.
Weather Lesson Four Moisture. ATMOSPHERIC MOISTURE Gaseous water is called WATER VAPOR. Major source of atmospheric water vapor is the OCEANS (70%). Sources.
Atmospheric Humidity.
Review Books Pages #s 1, 2, 3, 4, and 6.
HUMIDITY AND DEW POINT.
Water in the Air.
Humidity and Dew Point.
Temperature and Humidity
Do Now: Air rises ___________ and ____________
Atmospheric Moisture: Humidity
Unit 4 Weather ©Mark Place,
Aim: What is relative humidity?
Water & Humidity Earth Science – S1.
Spot the Differences (14)
How would you describe humidity in your own words?
Atmospheric Moisture Earth Science.
Water in the Atmosphere
Water’s Changes of State
Aim: What is relative humidity?
Water’s Changes of State
AIM: DO NOW: HW:.
Unit 4 Weather about Doppler Radar.
Water in the Atmosphere
Pick up worksheet from front table and glue into notebook.
Weather Part I Revised 2010 Revised 2010 ©Mark Place,
Draw this H L.
Humidity.
Dew Point and Cloud Formation
Humidity Water in the Air.
Humidity Water in the Air.
Dew Point and Cloud Formation
Humidity Water in the Air.
Spot the Differences (14)
Weather ©Mark Place,
Chapter 12 Section 3 How is relative humidity measured?
Humidity Water in the Air.
Humidity Water in the Air.
Humidity Water in the Air.
Humidity Water in the Air.
Chapter 12 Section 3 How is relative humidity measured?
Weather and Humidity 1.
How is relative humidity measured? What is the dew point?
6.3: Finding Moisture in the Atmosphere
Water in the Atmosphere
Moisture in the Atmosphere
Atmospheric Moisture Earth Science.
DYK: **The atmosphere contains only about 0.001% of the total volume of water on the planet (about 1.46 x 109 km3). **The rate at which water evaporates.
Presentation transcript:

L.O: SWBAT to determine dewpoint and relative humidity. Do Now: take your reference table, a PENCIL, and a scrap piece of paper (you can share (you only need half of the paper, must have 1 straight line) or grab one from the back by the printer.

When weather people know the relative humidity and the air’s dewpoint they can predict rain.

Dew Point Temperature Dew Point – The temperature at which air becomes saturated with water vapor.

When air is cooled to the dew point, condensation occurs. The dew point temperature depends on the amount of water vapor in the air. The closer the dew point gets to the temperature, the better the chance of precipitation. (*Important*)

Relative Humidity Relative Humidity – Compares the actual amount of water vapor in the air with the maximum amount of water vapor that the air can hold. (Tells you how much water vapor is in the air) Relative Humidity is expressed as a percent (%)

Relative Humidity is constantly changing Relative Humidity changes based on: 1) Temperature 2) The amount of water vapor

Relative Humidity & the Amount of H2O The Box can hold 20 molecules Relative Humidity & the Amount of H2O 20/20 15/20 10/20 5/20 100% 75% 50% 25%

Cold Air WARM AIR vs. Warm Air is Less Dense Cold Air is More Dense

Cold Air WARM AIR vs. Cold Air holds LESS Water Vapor Warm Air holds Warm Air is Less Dense Cold Air is More Dense Cold Air holds LESS Water Vapor Warm Air holds MORE Water Vapor

Relative Humidity & Temperature The amount of water vapor that air can hold depends on the temperature. Warm Air can hold more water vapor

When the relative humidity is near 100% , it rains When the relative humidity is near 100% , it rains! Because the air is saturated & it can’t hold anymore moisture!

Turn to ESRT pg 12. used to find dewpoint

This chart is used to calculate the relative humidity

this is a psychrometer: psychrometer is used to determine dew point and reletive humidity.

a Psychrometer is just two thermometers a Psychrometer is just two thermometers. One thermometer is called the “dry bulb”(can also be called air temperature), the other is called the “wet bulb”

How can we determine dewpoint temperatures? Step 1. WRITE OUT the wet bulb and the dry bulb temperatures. Step 2. Calculate the difference between wet bulb and dry bulb. (also known as the depression) Step 3. Take out your ESRT’s and turn to page 12

Step 4. Locate the dry bulb temperature reading on the left side of your chart. Step 5. Locate the difference between wet bulb and dry bulb on the top of your chart. Step 6. DRAW A LINE IN PENCIL TO DETERMINE THE DEW POINT!

1. If the dry bulb is 11oC and the wet bulb is 8oC. 2. What is the wet bulb temperature if dry bulb is 16oC and the dewpoint temperature is 9oC? 5 degrees C 12 degrees C

Relative Humidity You can determine the % Relative Humidity the SAME way you found the dewpoint temperature on the chart in the ESRT’s. What happens to the relative humidity as the air temperature approaches the dewpoint temperature? It increases!

Relative Humidity 1. What is the percent relative humidity if the Air Temperature is 20oC and the Wet Bulb is 11oC? 2. What is the percent relative humidity if the Dry-bulb temperature is 14oC and the Wet- bulb temperature is 14oC? 30% 100%

EXIT TICKET Fill in the chart EXIT TICKET Fill in the chart. Depression= difference between Wet&Dry bulb 4oC 24oC 72% 11oC 5oC 54% 17oC 15oC 20oC 74% 3oC 16oC 74.5%