Chapter #3, Question #13: Consider the following data for total atmospheric column ozone measurements (as DU) at three locations around the Earth, obtained using the TOMS in 2001. January 15 april 15 july 15 october 15 Tierra del fuego (Chilie, argentina) 323 261 339 206 Nairobi (Kenya) 234 273 266 (Aug. 15) 266 Kiev (Ukraine) 321 420 314 273 Assume that these are typical of values that might be obtained in any other year, and discuss the trends as you move down the columns and along the rows, in terms of your knowledge of stratospheric ozone behavior.

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Chapter #3, Question #13:

Consider the following data for total atmospheric column ozone measurements (as DU) at three locations around the Earth, obtained using the TOMS in 2001.

 

January 15

april 15

july 15

october 15

Tierra del fuego (Chilie, argentina)

323

261

339

206

Nairobi (Kenya)

234

273

266 (Aug. 15)

266

Kiev (Ukraine)

321

420

314

273

 

Assume that these are typical of values that might be obtained in any other year, and discuss the trends as you move down the columns and along the rows, in terms of your knowledge of stratospheric ozone behavior.

Expert Solution
Step 1

In the stratosphere, 85-90 % of total ozone present for the specific location above the surface. The measuring unit Dobson unit (DU) is used to calculated the thickness of ozone in the atmosphere. From the given data, Kiev has the relatively higher amount of ozone which is due to the fact that amount of ozone is higher almost all seasons at the middle and higher latitude.

Step 2

In the tropical region, such as Kenya, the lower amount of ozone and approximately same in all seasons, this can be explain using the Brewer-Dobson circulation model and according to this model, due to the slow atmospheric circulation, in which the ozone moves from tropic region to middle and polar latitudes.

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