Abstract. Ice-nucleating particles (INPs) are efficiently removed from
clouds through precipitation, a convenience of nature for the study of these
very rare particles that influence multiple climate-relevant cloud
properties including ice crystal concentrations, size distributions and
phase-partitioning processes. INPs suspended in precipitation can be used to
estimate in-cloud INP concentrations and to infer their original
composition. Offline droplet assays are commonly used to measure INP
concentrations in precipitation samples. Heat and filtration treatments
are also used to probe INP composition and size ranges. Many previous
studies report storing samples prior to INP analyses, but little is known
about the effects of storage on INP concentration or their sensitivity to
treatments. Here, through a study of 15 precipitation samples collected at a
coastal location in La Jolla, CA, USA, we found INP concentration changes up
to > 1 order of magnitude caused by storage to concentrations of
INPs with warm to moderate freezing temperatures (−7 to
−19 ∘C). We compared four conditions: (1) storage at room
temperature (+21–23 ∘C), (2) storage at +4 ∘C, (3) storage at −20 ∘C and (4) flash-freezing samples with liquid nitrogen prior to storage at −20 ∘C. Results demonstrate that storage can lead to both
enhancements and losses of greater than 1 order of magnitude, with
non-heat-labile INPs being generally less sensitive to storage regime, but
significant losses of INPs smaller than 0.45 µm in all tested storage
protocols. Correlations between total storage time (1–166 d) and changes
in INP concentrations were weak across sampling protocols, with the
exception of INPs with freezing temperatures ≥ −9 ∘C in samples stored at room temperature. We provide the
following recommendations for preservation of precipitation samples from
coastal or marine environments intended for INP analysis: that samples be
stored at −20 ∘C to minimize storage artifacts, that
changes due to storage are likely an additional uncertainty in INP
concentrations, and that filtration treatments be applied only to fresh
samples. At the freezing temperature −11 ∘C, average INP
concentration losses of 51 %, 74 %, 16 % and 41 % were observed for
untreated samples stored using the room temperature, +4, −20 ∘C, and flash-frozen protocols, respectively.
Finally, the estimated uncertainties associated with the four storage protocols
are provided for untreated, heat-treated and filtered samples for INPs
between −9 and −17 ∘C.