Remote sensing of NO2
Tropospheric NOx
Choose the correct option in each question. In some questions you can select multiple options.
About this exercise type...

The chemical lifetime of NOx in the boundary layer is approximately

1 hour
20 hours
6 hours
36 hours

The chemical lifetime of NOx in the upper troposphere is approximately

a few hours
several days to a week
a day
a month

The rapid breakdown of NOx leads to a large variation in its concentration. Urban areas can have concentrations in the order of

10 parts per billion by volume
10 parts per million by volume
10 parts per thousand by volume
10 parts per trillion by volume

whereas remote regions such as the upper troposphere and the boundary layers over remote areas of oceans can have concentrations in the order of

10 parts per billion by volume.
10 parts per million by volume.
10 parts per thousand by volume.
10 parts per trillion by volume.

The breakdown of NO2 can produce HNO3, which

permanently binds NOx.
acts as a temporary reservoir for NOx.
can itself be a source of NOx.
is only produced during daylight.

NB You can choose several options

During the day

HNO3 is rapidly photolysed.
Reacts directly with CH4 or other hydrocarbons.
HNO3 uses up NOx.

HNO3 acts as a sink for NO2

more during the day.
equally during night and day.
more during the night.
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