Top Banner
November 10, 2011
15

November 10, 2011

Feb 23, 2016

Download

Documents

zora

November 10, 2011. Objective: Determine Relative Humidity and dew point at various places around Riverheads HS. Agenda: Go over Relative Humidity/dew point worksheet Go over Test Lab: Relative Humidity Wind Notes. How to determine Dew Point & Humidity. Use a sling psychrometer: - PowerPoint PPT Presentation
Welcome message from author
This document is posted to help you gain knowledge. Please leave a comment to let me know what you think about it! Share it to your friends and learn new things together.
Transcript
Page 1: November 10, 2011

November 10, 2011

Page 2: November 10, 2011

Objective:Determine Relative

Humidity and dew point at various places around Riverheads HS

Agenda:Go over Relative

Humidity/dew point worksheet

Go over TestLab: Relative

HumidityWind Notes

Page 3: November 10, 2011

How to determine Dew Point & Humidity

Use a sling psychrometer:

1. Find the "dry bulb temp"

2. Subtract the dry and wet bulb.

3. Find the difference on the top

Use the exact same procedure for finding the Relative HumidityCHECK YOUR CHART!!

Page 4: November 10, 2011

Moving air is called Wind

231mph @ Mt. Washington, NHApril 12, 1934

http://www.mountwashington.org/about/visitor/recordwind.php

World's Strongest Wind:

Page 5: November 10, 2011

Wind

Basic Rules:

1. Warm air rises

2. There is always air

3. Warm air cools off

4. The Sun heats the GROUND

Wind is caused by differences in air

pressure

Page 6: November 10, 2011

Wind

Low Pressure

L

High Pressure

HWIND

Wind moves from

________________

to

________________

Remember that...

Page 7: November 10, 2011

WindWhich way is it moving??

Page 8: November 10, 2011

WindHow about here? ?

Page 9: November 10, 2011

Isomaps & Wind

Isobars:connect pointsof equal pressureThe closer the linesthe higher the windspeed.

http://ww2010.atmos.uiuc.edu/(Gh)/wx/surface.rxml

Think of contourmaps made of hills of air...

Page 10: November 10, 2011

There is always a more complex map

Page 11: November 10, 2011

Global Winds

Same thing; sideways and double

Warm air risesAi

r mov

es in

Air co

ols off

and s

inks

Page 12: November 10, 2011

wind is measured by an anemometer (wind speed) and a wind vane (direction)

Wind moves from areas of high pressure to areas of low pressure

Coriolis Effect: Because the earth is rotating, wind appears to curve.

In the northern hemisphere it curves to the right.

The Rules of Wind

Page 13: November 10, 2011
Page 14: November 10, 2011

Coriolis Effect

Because the Earth isrotating, the movementof objects appearsto curve.In the NORTH thecurve is to the right.

coriolis.mov

Page 15: November 10, 2011

Weather Instruments

Wind Vaneswind

direction

Thermometers

Temperature

BarometersAir

Pressure

AnemometersWind Speed

Leaning Tower of Pisa Mt. Washington -