In:
Atmospheric Measurement Techniques, Copernicus GmbH, Vol. 12, No. 11 ( 2019-11-08), p. 5879-5895
Abstract:
Abstract. Measuring vertical profiles of the particle light-absorption coefficient by
using absorption photometers may face the challenge of fast changes in
relative humidity (RH). These absorption photometers determine the particle light-absorption coefficient due to a change in light attenuation through a
particle-loaded filter. The filter material, however, takes up or releases
water with changing relative humidity (RH in %), thus influencing the light
attenuation. A sophisticated set of laboratory experiments was therefore conducted to
investigate the effect of fast RH changes (dRH ∕ dt) on the particle light-absorption coefficient (σabs in Mm−1) derived with two
absorption photometers. The RH dependence was examined based on different
filter types and filter loadings with respect to loading material and
areal loading density. The Single Channel Tricolor Absorption Photometer (STAP)
relies on quartz-fiber filter, and the microAeth® MA200 is
based on a polytetrafluoroethylene (PTFE) filter band. Furthermore, three
cases were investigated: clean filters, filters loaded with black carbon (BC),
and filters loaded with ammonium sulfate. The filter areal loading densities
(ρ*) ranged from 3.1 to 99.6 mg m−2 in the case of the STAP and
ammonium sulfate and 1.2 to 37.6 mg m−2 in the case the MA200.
Investigating BC-loaded cases, ρBC* was in the range of 2.9 to
43.0 and 1.1 to 16.3 mg m−2 for the STAP and MA200, respectively. Both instruments revealed opposing responses to relative humidity changes
(ΔRH) with different magnitudes. The STAP shows a linear dependence on
relative humidity changes. The MA200 is characterized by a distinct
exponential recovery after its filter was exposed to relative humidity
changes. At a wavelength of 624 nm and for the default 60 s running
average output, the STAP reveals an absolute change in σabs per absolute change of RH (Δσabs∕ΔRH) of 0.14 Mm−1 %−1 in the clean case, 0.29 Mm−1 %−1 in the case of BC-loaded filters, and 0.21 Mm−1 %−1 in the case filters loaded
with ammonium sulfate. The 60 s running average of the particle light-absorption coefficient at 625 nm measured with the MA200 revealed a response
of around −0.4 Mm−1 %−1 for all three cases. Whereas the
response of the STAP varies over the different loading materials, in
contrast, the MA200 was quite stable. The response was, for the STAP, in the
range of 0.17 to 0.24 Mm−1 %−1 and,
in the case of ammonium sulfate loading and in the BC-loaded case, 0.17 to 0.62 Mm−1 %−1. In the
ammonium sulfate case, the minimum response shown by the MA200 was −0.42 with a maximum of −0.36 Mm−1 %−1 and a minimum of −0.42 and maximum −0.37 Mm−1 %−1 in the case of BC. A linear correction function for the STAP was developed here. It is provided
by correlating 1 Hz resolved recalculated particle light-absorption
coefficients and RH change rates. The linear response is estimated at 10.08 Mm−1 s−1 %−1. A correction approach for the MA200 is also
provided; however, the behavior of the MA200 is more complex. Further
research and multi-instrument measurements have to be conducted to fully
understand the underlying processes, since the correction approach resulted
in different correction parameters across various experiments. However, the
exponential recovery after the filter of the MA200 experienced a RH change
could be reproduced. However, the given correction approach has to be
estimated with other RH sensors as well, since each sensor has a different
response time. And, for the given correction approaches, the uncertainties
could not be estimated, which was mainly due to the response time of the RH sensor.
Therefore, we do not recommend using the given approaches. But they
point in the right direction, and despite the imperfections, they are useful for at least estimating the measurement uncertainties due to relative humidity changes. Due to our findings, we recommend using an aerosol dryer upstream of
absorption photometers to reduce the RH effect significantly. Furthermore, when absorption photometers are used in vertical measurements, the ascending or
descending speed through layers of large relative humidity gradients has to be low to
minimize the observed RH effect. But this is simply not possible in some
scenarios, especially in unmixed layers or clouds. Additionally, recording
the RH of the sample stream allows correcting for the bias during post-processing of the data. This data correction leads to reasonable results,
according to the given example in this study.
Type of Medium:
Online Resource
ISSN:
1867-8548
DOI:
10.5194/amt-12-5879-2019
Language:
English
Publisher:
Copernicus GmbH
Publication Date:
2019
detail.hit.zdb_id:
2505596-3
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