FLOW Lab
- 2024-09-06T11:14:55-06:00
+ 2024-09-06T11:42:02-06:00http://flow.byu.eduAndrew Ning
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-Jekyll2024-09-06T11:14:55-06:00http://flow.byu.edu/feed.xmlFLOW LabFlight, Optimization, and Wind LaboratoryAndrew NingOptimization Book Available2021-10-15T00:00:00-06:002021-10-15T00:00:00-06:00http://flow.byu.edu/posts/opt-book]]>Andrew NingBEM Paper2021-07-30T00:00:00-06:002021-07-30T00:00:00-06:00http://flow.byu.edu/posts/bem-paper]]>Andrew NingEduardo Research Update2021-03-01T00:00:00-07:002021-03-01T00:00:00-07:00http://flow.byu.edu/posts/eduardo-latest]]>Eduardo AlvarezReformulated VPM2021-02-01T00:00:00-07:002021-02-01T00:00:00-07:00http://flow.byu.edu/posts/reformulated-vpm]]>Eduardo AlvarezOptimization Book Announcement2021-01-20T00:00:00-07:002021-01-20T00:00:00-07:00http://flow.byu.edu/posts/optimization-book]]>Andrew NingPJ Defense2020-09-30T00:00:00-06:002020-09-30T00:00:00-06:00http://flow.byu.edu/posts/pj-defense]]>Andrew NingVPM Paper2020-08-30T00:00:00-06:002020-08-30T00:00:00-06:00http://flow.byu.edu/posts/vpm-paper]]>Eduardo AlvarezAirborne Wind with Vortex Particle Method2020-08-16T00:00:00-06:002020-08-16T00:00:00-06:00http://flow.byu.edu/posts/wind-harvesting]]>Judd Mehr and Eduardo AlvarezEduardo’s Past Three Years2020-08-10T00:00:00-06:002020-08-10T00:00:00-06:00http://flow.byu.edu/posts/eduardo-three-years]]>Eduardo AlvarezFLOWUnsteady in Google Drive2020-08-02T00:00:00-06:002020-08-02T00:00:00-06:00http://flow.byu.edu/posts/google-drive-vpm]]>Eduardo Alvarez
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+Jekyll2024-09-06T11:42:02-06:00http://flow.byu.edu/feed.xmlFLOW LabFlight, Optimization, and Wind LaboratoryAndrew NingOptimization Book Available2021-10-15T00:00:00-06:002021-10-15T00:00:00-06:00http://flow.byu.edu/posts/opt-book]]>Andrew NingBEM Paper2021-07-30T00:00:00-06:002021-07-30T00:00:00-06:00http://flow.byu.edu/posts/bem-paper]]>Andrew NingEduardo Research Update2021-03-01T00:00:00-07:002021-03-01T00:00:00-07:00http://flow.byu.edu/posts/eduardo-latest]]>Eduardo AlvarezReformulated VPM2021-02-01T00:00:00-07:002021-02-01T00:00:00-07:00http://flow.byu.edu/posts/reformulated-vpm]]>Eduardo AlvarezOptimization Book Announcement2021-01-20T00:00:00-07:002021-01-20T00:00:00-07:00http://flow.byu.edu/posts/optimization-book]]>Andrew NingPJ Defense2020-09-30T00:00:00-06:002020-09-30T00:00:00-06:00http://flow.byu.edu/posts/pj-defense]]>Andrew NingVPM Paper2020-08-30T00:00:00-06:002020-08-30T00:00:00-06:00http://flow.byu.edu/posts/vpm-paper]]>Eduardo AlvarezAirborne Wind with Vortex Particle Method2020-08-16T00:00:00-06:002020-08-16T00:00:00-06:00http://flow.byu.edu/posts/wind-harvesting]]>Judd Mehr and Eduardo AlvarezEduardo’s Past Three Years2020-08-10T00:00:00-06:002020-08-10T00:00:00-06:00http://flow.byu.edu/posts/eduardo-three-years]]>Eduardo AlvarezFLOWUnsteady in Google Drive2020-08-02T00:00:00-06:002020-08-02T00:00:00-06:00http://flow.byu.edu/posts/google-drive-vpm]]>Eduardo Alvarez
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diff --git a/me275/schedule/hw1/index.html b/me275/schedule/hw1/index.html
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@@ -107,16 +107,13 @@
HW 1
Create a function called patriot() that returns your answer in meters.
-
1.2 In aerospace applications we need a model of atmospheric properties. The International Standard Atmosphere provides a common reference for temperature and pressure as a function of altitude. The temperature varies in altitude (where \(T\) is in Kelvin and \(h\) is in km) as:
+
1.2 In aerospace applications we need a model of atmospheric properties. The International Standard Atmosphere provides a common reference for temperature and pressure as a function of altitude. The temperature varies in altitude (where \(T\) is in Kelvin and \(h\) is in km) as (we’ll only go up to 47 km for brevity):
\[T(h) = \begin{cases}
288.15 - 6.5 h & 0 < h < 11 \text{ km} \\
216.65 & 11 < h < 20 \text{ km} \\
-216.65 + h & 20 < h < 32 \text{ km} \\
-228.65 + 2.8 h & 32 < h < 47 \text{ km} \\
-270.65 & 47 < h < 51 \text{ km} \\
-270.65 -2.8 h & 51 < h < 71 \text{ km} \\
-214.65 -2 h & 71 < h < 84 \text{ km} \\
+216.65 + (h - 20) & 20 < h < 32 \text{ km} \\
+228.65 + 2.8 (h - 32) & 32 < h < 47 \text{ km} \\
\end{cases}\]
Plot the temperature as a function of altitude. Normally we put the dependent variable on the \(y\)-axis, but in this case it usually makes interpretation easier to plot altitude on the \(y\) axis (since it is vertical). Be sure to add appropriate labels and units.