Cold Case Model Hot Case Model GPS LMC GPS LMC Launch

Slides:



Advertisements
Similar presentations
Topic: How Climate Affects Us
Advertisements

WEATHER.
Bare rock model Assumptions
17.2 Heating the Atmosphere
Sandy desert Modifications of the surface radiation budget.
MET 61 1 MET 61 Introduction to Meteorology MET 61 Introduction to Meteorology - Lecture 9 “Radiative Transfer” Dr. Eugene Cordero Stull: Chapter 2 Class.
Solar constant The solar constant is the amount of incoming solar radiation per unit area, measured on the outer surface of Earth's atmosphere, in a plane.
Atmospheric Chemistry Global Warming. GasMole Percent N O Ar0.934 CO O3O3 1.0 x Composition of Atmosphere:
1 Aerospace Thermal Analysis Overview G. Nacouzi ME 155B.
AgWeatherNet Annual Note: Be sure you have already selected your station before choosing this product. Select AWN Reports Click on Annual.
Lesson 2 AOSC 621. Radiative equilibrium Where S is the solar constant. The earth reflects some of this radiation. Let the albedo be ρ, then the energy.
Thermal Modeling of the CX Satellite Jacob Boettcher Thermal Team Lead 4/5/02.
Atmospheric Chemistry Global Warming. GasMole Percent N O Ar0.934 CO O3O3 1.0 x Composition of Atmosphere:
Introduction to Climate Prediction Find out what happens to radiation from the Sun when it gets to the Earth, and what this means for the planet’s temperature.
FASTRAC Thermal Model Analysis By Millan Diaz-Aguado.
Weather and Climate Part 1 - Introduction CGF3M Crescent School.
EGU General Assembly C. Cassardo 1, M. Galli 1, N. Vela 1 and S. K. Park 2,3 1 Department of General Physics, University of Torino, Italy 2 Department.
FACTORS INFLUENCING CLIMATE NOVEMBER 18, MAIN FACTORS THAT INFLUENCE CLIMATE Latitude Mountain and Elevation Water bodies Moving air Ocean Currents.
The day after solar cycle 23 IHY 2009 September 23, 2009 Yu Yi 1 and Su Yeon Oh 2 1 Dept. of Astronomy & Space Science, Chungnam National University, Korea.
Objective: To know that climate is often defined by annual temperatures and precipitation amounts.
AOS February 19/21 Energy Transfer. Four mechanisms of transfer Conduction Convection Advection Radiation.
Albedo varies with season and geography Surface cover that has a high albedo Snow & ice Cloud cover Aerosols 
The Atmosphere: Part 8: Climate Change: Sensitivity and Feedbacks Composition / Structure Radiative transfer Vertical and latitudinal heat transport Atmospheric.
DAILY INSOLATION OVER THE YEAR AT VARIOUS LATITUDES (NORTH HEMISPHERE)
Global Warming. GasMole Percent N2N O2O Ar0.934 CO O3O3 1.0 x Composition of Atmosphere:
Proprietary BalloonWinds Update Author: Ivan Dors – UNH Presented By: Michael Dehring -- MAC 28 June 2006.
Goals for Today 1.PREDICT the consequences of varying the factors that determine the (a) effective radiating temperature and (b) mean surface temperature.
Predicting Near Space Flights L. Paul Verhage 13 July 2013.
Thermal Control Subsystem
Geography Antarctica How Cold is Antarctica and why?[Date] Today I will: - Be able to work out the range of world temperatures - Be able to explain why.
Climate and Global Change Notes 17-1 Earth’s Radiation & Energy Budget Resulting Seasonal and Daily Temperature Variations Vertical Temperature Variation.
Chapter 3.4 Notes Thermal Rates.  The amount of heat that is transferred per unit time is the heat flow rate  Equation for heat flow rate = heat / time.
Climate Modeling In -Class Discussion: Energy Balance Models.
Unique Properties of the Earth. 1. Due to the location in the solar system the Earth is not too hot and not too cold… it’s just right for life.
* Materials that allow heat, electricity, or sound waves to pass through them.
TEM – Lecture 5 Radiative Heat Flow. Radiation Radiation intensity increases with temperature! Every surface above zero K Radiates!
Date of download: 10/15/2017 Copyright © ASME. All rights reserved.
Chapter 17: The Atmosphere
Date of download: 10/16/2017 Copyright © ASME. All rights reserved.
Heating the Earth’s Surface
Ice-Cold Lemonade It was a hot summer day. Mattie poured herself a glass of lemonade. The lemonade was warm, so Mattie put some ice in the glass. After.
Reasons for the Seasons
PRELIMINARY MAP - Sun On Secondary Reflector Analysis #4
Preliminary MAP - Sun On Secondary Reflector Analysis #3
Jason Link University of Hawaii
What is Climate?.
Insolation In = incoming Sol = solar Ation = radiation Insolation – radiation from the sun.
Warm-up September 1st Answer the following questions with your partner on a piece of paper to turn in: What are the 5 stages to the water cycle? How do.
TEM – Lecture 5 Radiative Heat Flow.
L.O: SWBAT explain RADIATIVE BALANCE; how the amount of insolation an area receives, gives off affects its climate and explain DURATION OF INSOLATION (length.
Earth-Sun Relationships
Chapter 17.3 Temperature Controls.
Heating of the Earth Energy Transfers
Thursday 4/27/17 Notebook Entry: What was one thing you learned from the Season Simulation you looked at yesterday? What is one thing you found difficult.
Globe Skills.
L.O: SWBAT explain why the angle of insolation (angle of sunlight) gives Earth its climates and seasons.
What is Climate?.
D46 Convection Currents.
Insolation.
JOSH STAMPS ROBIN HEGEDUS
LRO CRaTER Preliminary Temperature Predictions Design A Concept  Old Concept April 12, 2005 Cynthia Simmons/ESS.
Warm Up 10 4/6 Write about your spring break.
Friday 4/28/17 No Notebook Entry
Thermodynamics Atmosphere
Section Thermal Energy Transfer
Begin working on the winds worksheet from the quiz day.
Catalyst 4/9 Why does someone in Brazil experience different climate than someone in the Ventura Area?
By: Inigo Gabriel Gutierrez
A Presentation by _________
Conversations with the Earth Tom Burbine
Presentation transcript:

Cold Case Model Hot Case Model GPS LMC GPS LMC Launch 4.7 QCL LO Cryocooler OFF Ascent 4.7 QCL LO Cryocooler ON Predictions of the Cooling fluid temperature at the inlet of the radiator for two environmental model cases. The parameters for the two cases are in the next slide This model assumes that the cryocooler used to cool the 4.7THz QCL is turned ON for ONLY 2 hours during the second day at about 2 hours prior to changing attitude to look at the LMC. It is turned OFF when moving to the LMC Cooling system input power assumptions: 260 W when 4.7 THz is NOT in use, 500W when it is in use.

Hot and Cold cases simulations Hot Case Float altitude 120 kft Latitude 70° S Date Jan 31st Dec 21st Solar Flux 1392 W/m2 1397 W/m2 Albedo 63% 95% Earth Flux of 156 W/m2 250 W/m2 For both Cold and Hot cases runs the model simulates dynamically prelaunch, ascent, and first 48 hours of flight with predicted gondola attitude and telescope elevation