FC chemistry in the stratosphere Flashcards

1
Q

What percentage of O3 is found in the stratosphere

A

90%

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2
Q

Which species dominates stratosphere chemistry

A

O3 and O dominate stratospheric chemistry in the same way OH radicals dominate in the troposphere

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3
Q

Describe how O3 is produced in the stratosphere

A

O3 is produced photochemically, together with O in a cyclic process described by the chapman model

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4
Q

Compare and contrast chemistry in the stratosphere with chemistry in the troposphere

A

Species that survive physical losses and chemical conversions in the troposphere (N2O, CH4 and CH3Cl) are transported into the stratosphere where they yield the NOx, HOx and ClOx radicals that destroy O3.
Stratospheric chemistry is simple yet involves about 50 chemical species in nearly 200 reactions way more than the troposphere

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5
Q

What sort of substance is ozone

A

An endothermic substance

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6
Q

What type of reactions are those involving ozone

A

Reactions involving ozone are often exothermic and rates tend to be high, even more when it absorbs light.

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7
Q

Describe O3 formation in daylight hours

A

During daylight hours there is more photodisociation of O3 and O2 so there is more O2 and O species combining to make O3.
O3 has a very short photolysis lifetime during the day

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8
Q

Describe O3 formation at night

A

No photodissociation, so O and O(¹D) recombine or react, reducing odd oxygen concentrations. Reservoir species (NO₂, ClONO₂) become important in storing reactive species.

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9
Q

Describe the O3 chemistry at increasing altitudes

A

At increasing altitudes solar intensity is high but [O2] get low, therefore the formation of O3 gets slower but the [O]/[O3] gets higher

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10
Q

What is the main source of O species in the stratosphere

A

The source of the photolysis of O2 by short wavelength UV radiation

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11
Q

Describe the O3 chemistry at low altitudes

A

At low altitudes there is plenty of [O2] concentration but less radiation to dissociate it. Less UV radiation penetrates, leading to less ozone formation.

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