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Pressure Conversion The pascal (Pa) is the international standard unit for pressure. It is named after French mathematician, Blaise Pascal (1623-1662), for his experiments with ... 2.
Atmospheric Visualization Collection: Student Produced Weather Reports Thanks to the Internet, affordable school weather stations, ... Having students produce their own classroom weather reports is an enjoyable and highly ... 3.
Atmospheric Visualization Collection: Atmospheric Visualization ... Atmospheric Visualization Collection ... Stable revisions will be displayed on our collection's [lesson plan page]. Our current lesson plans include: ... 4.
Atmospheric Visualization Collection: Noon Shadows On The Equinox Sep 24, 2003 ... Mount several meter sticks on a classroom wall, one representing the vertical meter stick casting the shadow, and the others measuring ... 5.
Atmospheric Visualization Collection: Cloud Base Model This java applet,[A Cloud Base Model], was created by Steve Ackerman and Tom Whittaker at the University of Wisconsin with free use for non-profit ... 6.
Atmospheric Visualization Collection: Weather Radar In A Shoe Box Distribute a shoe box and lid, 2 copies of the graph paper, and all other materials to each team. Inside each box the students will use the items of various ... 7.
NSDL: Weather Radar In A Shoe Box 1 cm x 1 cm square graph paper to cover shoe box lid ... Once secured, the students should tape the lids on the shoe boxes and trade them with those built ... 8.
Atmospheric Visualization Collection: Hurricane Houses 60 cm cellophane tape. scissors. calculator. formulae for determining volume of various geometric shapes. metric ruler. safety goggles. Teacher -. stopwatch ... 9.
Atmospheric Visualization Collection: Getting Started With The ... In this case we?re using this capability to allow teachers interactively modify lesson plans, which we call our Lesson Plan Sandbox. ... 10.
NSDL: An Introduction To Heat Index The following formula is used to calculate the Heat Index (HI) where T = Air Temperature in °F and RH = Relative Humidity in %. Using T, RH and the formula ... |
