An amount of energy from the Sun is intercepted by the Earth. While almost this amount of energy is ultimately radiated back to space, Earth’s spherical shape and rotation causes local imbalance between incoming and outgoing radiation. This discrepancy gives rise to motions. Understanding the structure and dynamics of the atmosphere is central to forecasting weather and understanding climate. This course aims to build a fundamental set of physical principles and apply them to understanding large-scale atmospheric motions. Mathematical descriptions of the atmospheric dynamics are constructed and interpreted in terms of their physical significance. By the end of this course we will have investigated phenomena such as the thermodynamics of the atmosphere, forces in the atmosphere planetary waves, mid-latitude cyclones, the planetary boundary layer, and aspects of the general circulation of the atmosphere.
Time:
Fall 2012, Tuesday/Thursday, 11:00am
-12:15pm
Web Page:
http://atoc.colorado.edu/~dcn/ATOC5050
Instructor:
David Noone,
Ekeley S236, 303-735-6073 (dcn@colorado.edu)
Office hours:
Tuesdays 1-2pm and 3:15-5pm, or by appointment.
(Also R. R. Rogers and M. K. Yau, A
Short Course in Cloud Physics, 3rd Ed., Butterworth and
Heinemann, 1989,
and/or J. M. Wallace and P. V. Hobbs,
Atmospheric Science, 2nd ed., Elsevier, 2006.
|
Holton, J. R., An introduction of Dynamic Meteorology, Elsevier Academic Press, 4th
ed., 2004. |
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Rogers, R. R., and M. K. Yau, A short course in cloud physics, Butterworth and
Heinemann, 3rd ed., 1989. |
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Download a copy of the syllabus.
Approximate lecture outline.
| Week | # | Date | Topics | Reading | Assign | Notes |
| I | 1 | 28 Aug | Introduction and overview | H Ch1.1-1.3 | ||
| 2 | 30 Aug | Pressure and hydrostatic | H 1.4-1.5, RY1 | |||
| II | 3 | 04 Sep | Thermodynamic EQ and adiabatic processes | H2, RY2 | ||
| 4 | 06 Sep | Dry adiabatic processes | RY2, H Ch9 | |||
| III | 5 | 11 Sep | Water and saturation | RY3 | ||
| 6 | 13 Sep | Moist adiabatic processes | RY3 | |||
| IV | 7 | 18 Sep | Stability and buoyancy | H2 | ||
| 8 | 20 Sep | Instability and conditions | H2 | |||
| V | 9 | 25 Sep | Advection and balance flow | H2 | ||
| 10 | 27 Sep | Review session, homework tutorial: EKELEY W231 | H2 | HW1 due | ||
| VI | 11 | 02 Oct | Geostrophic balance and Coriolis force | H3 | ||
| 12 | 04 Oct | Continuity and MJO | H2 | |||
| VII | 13 | 09 Oct | Thermal wind balance | H2 | ||
| 14 | 11 Oct | Midterm | ||||
| VIII | 15 | 16 Oct | Balanced flow | H3 | ||
| 16 | 18 Oct | Balanced flow - lab experiments | H3 | Coriolis demo class worksheet | ||
| IX | 17 | 23 Oct | Balanced flow - asymmetry and thermal | H3 | ||
| 18 | 25 Oct | Divergence and vorticity | H4 | |||
| X | 19 | 30 Oct | Circulation theorem | H4 | Vorex demo | |
| 20 | 01 Nov | Vorticity and conservation of PV | H4 | Taylor column demo | ||
| XI | 21 | 06 Nov | Vorticity equation and scaling | H4 | ||
| 22 | 08 Nov | Vorticity (Rossby) waves | H4, and 7.7 | HW2 due | ||
| XII | 23 | 13 Nov | Boundary layers 1 - eke and Richardson number | H5 | Purple water demo | |
| 24 | 15 Nov | Field trip - DATA AVAILABLE BELOW | H5 | Field assignment sheet | ||
| XIII | 20 Nov | Thanksgiving - no class | ||||
| 22 Nov | Thanksgiving - no class | |||||
| XIV | 25 | 27 Nov | Boundary layers 3 - surface layer and the mixing length | H5 | ||
| 26 | 29 Nov | Boundary layers 4 - Ekman layers, spin down | H5 | Project due, HW3 assignment | ||
| XV | 27 | 04 Dec | Optional lab work with Scott (no lecture) | |||
| 28 | 06 Dec | Exam | ||||
| XVI | 29 | 11 Dec | Geostrophic adjustment | H6,7.6 | ||
| 30 | 13 Dec | Zonal mean circulation/baroclinic instability | H7, 10, extra reading | See
movies below HW3 due (Friday!) |
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| Exam | ||||||
Homework assignment 1 (Due 27 Sept): Download assignment.
Homework assignment 2 (Due 8 Nov): Download assignment
Data analysis project (Due 29 Nov): Download assignment
Homework assignment 3 (Due 14 Dec): Download assignment
Field data
Combined excel file containing all balloon theodolite angles (note, waiting for 1 group): ATOC 5050_all_balloons.xls
Raw data files for wind an temperature in csv format, or a excel file containing both: ATOC 5050_tower_data.xls
Also, a manual for the micromet tower.
Remember, tower sensor heights were 0.7, 1.5, 3.0 and 6.49 meters. Columns labeled levels 1 to 4 is bottom and 4 is the top. Wind directions is only at the top.
Also remember that the date stamp in the data files is wrong, because we did not set the clock. The tower data file contains 1 hour of data, and you only need to consider four 10-minute averages (so, 40 minutes of data).
Photos! HERE is a directory with photos from the field trip. (If you have others you'd like to share send them along and I'll add them to the directory)
Precipitable water from CAM2 shows tropical easterlies and westerly "river" storms.
Baroclinic annulus: no rotation shows flow toward cold center at the top of the fluid
Baroclinic annulus: "earth like" rotation shows (bright) just, and onset of waves with change in rotation rate
Baroclinic annulus: other examples - three, four, five
Spin up of CAM from state initially at rest, with a tiny mountain (fli files can be viewed with quicktime)
As above, but zoomed in on mountain
Done!