Air quality expert group - Fine particulate matter (PM2.5) in ... - Defra
Air quality expert group - Fine particulate matter (PM2.5) in ... - Defra
Air quality expert group - Fine particulate matter (PM2.5) in ... - Defra
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<strong>PM2.5</strong> <strong>in</strong> the UK<br />
46<br />
3.2.1 Diurnal variations of <strong>PM2.5</strong> at urban background sites<br />
4. The diurnal cycle of <strong>PM2.5</strong> dur<strong>in</strong>g 2010 is summarised <strong>in</strong> Figure 3.1a for four<br />
areas of the UK. Concentrations have been averaged by hour of the day<br />
us<strong>in</strong>g local time, i.e. they take account of the change from w<strong>in</strong>ter to summer<br />
time. The plots show average concentrations for the hour beg<strong>in</strong>n<strong>in</strong>g the<br />
measurement period, i.e. the value shown for 23:00 is the average over the<br />
period 23:00 to 24:00. The concentration scale is the same on all the urban<br />
background plots. The del<strong>in</strong>eation of the four areas is shown <strong>in</strong> Figure 3.1b.<br />
The diurnal cycle is fairly limited <strong>in</strong> scale, spann<strong>in</strong>g just a few µg m -3 . The central<br />
UK, southern UK and London sites have a very similar pattern, with the lowest<br />
concentrations occurr<strong>in</strong>g dur<strong>in</strong>g the afternoon, between 13:00 and 17:00.<br />
They also show a morn<strong>in</strong>g peak, around 08:00-09:00, and a late even<strong>in</strong>g peak,<br />
around 21:00. The concentrations at the northern UK sites are lower overall than<br />
those <strong>in</strong> the other three areas. There is also no afternoon dip <strong>in</strong> concentrations<br />
at the northern UK sites; the lowest concentrations thus occur dur<strong>in</strong>g the early<br />
morn<strong>in</strong>g period, around 04:00-06:00. This observation is consistent with the<br />
lesser role played by secondary nitrates <strong>in</strong> the north of the UK.<br />
5. Figure 3.2 shows dist<strong>in</strong>ct differences <strong>in</strong> the diurnal patterns for w<strong>in</strong>ter and<br />
summer at southern UK sites <strong>in</strong> 2010, although the lowest concentrations still<br />
occur dur<strong>in</strong>g the afternoon <strong>in</strong> both seasons. The w<strong>in</strong>ter concentrations show<br />
more substantial morn<strong>in</strong>g and late even<strong>in</strong>g peaks than do the summer values,<br />
which may be related to greater domestic heat<strong>in</strong>g requirements at these times<br />
of day. These patterns are essentially the same as those reported for 2009<br />
by Laxen et al. (2010), who also analysed the diurnal patterns for nitrate, as<br />
well as those for the volatile component of <strong>PM2.5</strong>, as def<strong>in</strong>ed by the FDMS<br />
analysers. They concluded that the afternoon dip was probably due to the loss<br />
of the semi-volatile nitrate particles dur<strong>in</strong>g the warmer afternoon period. The<br />
morn<strong>in</strong>g peak was probably related to road traffic and domestic emissions,<br />
with the late even<strong>in</strong>g peak probably related to domestic sources, both from<br />
heat<strong>in</strong>g and cook<strong>in</strong>g. The l<strong>in</strong>k with heat<strong>in</strong>g can also be seen <strong>in</strong> the results for<br />
black carbon <strong>in</strong> Figure 3.23. Laxen et al. (2010) also considered that the even<strong>in</strong>g<br />
peak may <strong>in</strong> part be due to reduced dispersion aris<strong>in</strong>g from the more stable<br />
atmospheric conditions dur<strong>in</strong>g the night, together with a contribution from<br />
volatile <strong>particulate</strong> <strong>matter</strong> (PM) (i.e. nitrate and organic compounds) condens<strong>in</strong>g<br />
on ambient particles at lower night-time temperatures. The average diurnal <strong>PM2.5</strong><br />
ranges are nevertheless relatively small, around 5 µg m -3 <strong>in</strong> w<strong>in</strong>ter and 2 µg m -3<br />
<strong>in</strong> summer, relative to the seasonal mean concentrations of around 17 µg m -3 <strong>in</strong><br />
w<strong>in</strong>ter and 11 µg m -3 <strong>in</strong> summer, suggest<strong>in</strong>g that local sources are not dom<strong>in</strong>ant.