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Published byAugustus Harmon Modified over 9 years ago
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Team Philosoraptors: Temperature, Humidity, Pressure Hannah Gardiner Joe Valieant Bill Freeman Randy Dupuis
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Goals and Objectives Goals Objectives
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Science Objectives Layers of the atmosphere Time dependence
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Technical Objectives Payload Money and Weight Measurements Documentation PDR CDR FRR
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Earth’s Atmosphere
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Overview Troposphere Troposphere – Clouds Stratosphere Stratosphere Mesosphere Mesosphere Thermosphere Thermosphere
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Troposphere Atmospheric Conditions “Stirring”
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Clouds
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Stratosphere Atmospheric Conditions Ozone Layer
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Mesosphere Atmospheric Conditions Measuring
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Thermosphere Atmospheric conditions Start of “space”
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Review Atmospheric layers
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Weather Balloons http://www.ehow.com/about_5050060_history-weather-balloons.html
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Science Background
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US Model Atmosphere 1976 Produced by NOAA, NASA, and USAF – NOAA: National Oceanic and Atmospheric Administration – NASA: National Aeronautics and Space Administration – USAF: United States Air Force
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US Model Atmosphere 1976 Theoretical model of the atmosphere using: – Ideal gas law p = DRT – Hydrostatic Equilibrium law dp/dh = -gD p = Pressure of air D = Density of air R = Universal Gas Constant T = Temperature g = Acceleration due to gravity
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US Model Atmosphere 1976 Assumes: – Dry Air – Temperature is linear with altitude Can calculate properties of the atmosphere – Pressure – Temperature – Density – Speed of sound
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Measured Temperature profile of the atmosphere TroposphereTropopauseStratosphere
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Measured Lapse Rate of the atmosphere TroposphereTropopauseStratosphere
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Measured and theoretical pressure as a function of altitude TroposphereTropopauseStratosphere
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Measured humidity as a function of altitude TroposphereTropopauseStratosphere
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Measured humidity rate of change as a function of altitude TroposphereTropopauseStratosphere
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Temperature error and humidity as a function of altitude in the Troposphere
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Science Requirements Temperature Pressure Humidity -70 °C 30 °C 10 Pressure Sensor (atm) 0% 100%
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Technical Requirements Payload must cost less than $500 and weigh less than 500 grams. Payload must have separate sensors to measure pressure, temperature, and humidity and a real time clock to timestamp data. Signal conditioning is required to transform the signal from the sensor to a signal that spans the range of the ADC on the BalloonSat. The payload must have enough memory available to take data every 10 seconds.
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Sensor Information The payload must have temperature sensors that to measure temperatures between 30 and -70 °C on the inside and outside of the payload with a standard deviation of ± 1.7 °C The payload must have a pressure sensor to measure pressures between 1 and 0.008 atm with a standard deviation of ± 0.002 atm The payload must have a humidity sensor to measure humidity between 100 and 0 %rel with a standard deviation of ± 0.5 %rel
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Temperature Sensors There are 2 different types contact and noncontact. Contact Sensors function by producing an electrical output based on the temperature of the sensor. These sensors are placed in contact with the target and if the sensor and target are in thermal equilibrium (no heat flow between the sensor and target) the target’s temperature can be measured Noncontact Sensors measure temperature using the thermal radiant power of the infrared or optical radiation from the targets surface. Some examples are Thermocouples, thermistor, RTD’s
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Pressure Sensors Pressure sensors are mechanical elements that are designed to deflect when pressure is applied. The deflection can be measured and transduced to produce an electrical output. Examples include poteniometric, piezoressistive, capacitive, and piezoelectric sensors
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Humidity Sensors There are three main types: capacitive, resistive, and thermal conductive. Capacitive sensors consist of a substrate with a thin film placed in between two conductive electrodes, as the relative humidity changes the capacitance changes. Resistive sensors measure the change in the impedance of a hygroscpoic medium. Thermal Conductive sensors measure the absolute humidity by using the difference of the thermal conductivity of dry air and air containing water vapor
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