Production of ice-nucleating particles (INPs) by fast-growing phytoplankton

Thornton, Daniel C. O.; Brooks, Sarah D.; Wilbourn, Elise K.; Mirrielees, Jessica; Alsante, Alyssa N.; Gold-Bouchot, Gerardo; Whitesell, Andrew; McFadden, Kiana

doi:10.5194/acp-23-12707-2023

Production of ice-nucleating particles (INPs) by fast-growing phytoplankton

Journal Article · Wed Oct 11 00:00:00 EDT 2023 · Atmospheric Chemistry and Physics (Online)

DOI:https://doi.org/10.5194/acp-23-12707-2023· OSTI ID:2251610

^[1]; Brooks, Sarah D. ^[1]; Wilbourn, Elise K. ^[1]; Mirrielees, Jessica ^[1]; Alsante, Alyssa N. ^[1]; ^[1]; Whitesell, Andrew ^[2]; McFadden, Kiana ^[3]

Texas A & M University, College Station, TX (United States)
Texas A & M University, College Station, TX (United States); North Carolina State University, Raleigh, NC (United States)
Texas A & M University, College Station, TX (United States); Jackson State University, MS (United States)

Sea spray aerosol contains ice-nucleating particles (INPs), which affect the formation and proper ties of clouds. Here, we show that aerosols emitted from fast-growing marine phytoplankton produce effective immersion INPs, which nucleate at temperatures significantly warmer than the atmospheric homogeneous freezing (-38.0 °C) of pure water. Aerosol sampled over phytoplankton cultures grown in a Marine Aerosol Ref erence Tank (MART) induced nucleation and freezing at temperatures as high as -15.0 °C during exponential phytoplankton growth. This was observed in monospecific cultures representative of two major groups of phy toplankton, namely a cyanobacterium (Synechococcus elongatus) and a diatom (Thalassiosira weissflogii). Ice nucleation occurred at colder temperatures (-28.5 °C and below), which were not different from the freezing temperatures of procedural blanks, when the cultures were in the stationary or death phases of growth. Ice nucleation at warmer temperatures was associated with relatively high values of the maximum quantum yield of photosystem II (^Φ_PSII), an indicator of the physiological status of phytoplankton. High values of ^Φ_PSII indicate the presence of cells with efficient photochemistry and greater potential for photosynthesis. For comparison, field measurements in the North Atlantic Ocean showed that high net growth rates of natural phytoplankton assemblages were associated with marine aerosol that acted as effective immersion INPs at relatively warm temperatures. Data were collected over 4 d at a sampling station maintained in the same water mass as the water column stabilized after deep mixing by a storm. Phytoplankton biomass and net phytoplankton growth rate (0.56 d^-1) were greatest over the 24 h preceding the warmest mean ice nucleation temperature (-25.5 °C). Collectively, our laboratory and field observations indicate that phytoplankton physiological status is a useful predictor of effective INPs and more reliable than biomass or taxonomic affiliation. Ocean regions associated with fast phytoplankton growth, such as the North Atlantic during the annual spring bloom, may be significant sources of atmospheric INPs.

View Accepted Manuscript (DOE)

Research Organization:: Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)

Sponsoring Organization:: USDOE; National Science Foundation (NSF); National Aeronautics and Space Administration (NASA)

Grant/Contract Number:: AC05-00OR22725

OSTI ID:: 2251610

Journal Information:: Atmospheric Chemistry and Physics (Online), Journal Name: Atmospheric Chemistry and Physics (Online) Journal Issue: 19 Vol. 23; ISSN 1680-7324

Publisher:: Copernicus Publications, EGUCopyright Statement

Country of Publication:: United States

Language:: English

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