Seasonal Variation of Wet Deposition of Black Carbon at Ny‐Ålesund, Svalbard
Open Access
- 16 June 2021
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Atmospheres
- Vol. 126 (12)
Abstract
Black carbon (BC) aerosol deposited in and onto Arctic snow increases the snow's absorption of solar radiation and accelerates snowmelt. Concentrations of BC in the Arctic atmosphere and snow are controlled by wet deposition; however, details of this process are poorly understood owing to the scarcity of time‐resolved measurements of BC in hydrometeors. We measured mass concentrations of BC in hydrometeors (CMBC) and in air (MBC) with 16% and 15% accuracies, respectively, at Ny‐Ålesund, Svalbard during 2012–2019. Median monthly MBC and CMBC values showed similar seasonal variations, being high in winter‐spring and low in summer. Median monthly BC wet deposition mass flux (FMBC) was highest in winter and lowest in summer, associated with seasonal patterns of CMBC and precipitation. Seasonally averaged BC size distributions in hydrometeors were similar except for summer. Measurements of MBC and CMBC in spring 2017 showed a size‐independent removal efficiency, indicating that BC‐containing particles were efficiently activated into cloud droplets. These observations at Ny‐Ålesund were compared with observations at Barrow, Alaska, during 2013–2017. The near‐surface MBC at Ny‐Ålesund and Barrow had similar seasonal patterns; however, the two sites differed in CMBC and FMBC. In summer, CMBC was low at Ny‐Ålesund but moderate at Barrow, likely reflecting differences in MBC in the lower troposphere. Seasonally averaged BC size distributions in hydrometeors were similar at both sites, suggesting that average BC size distributions are similar in the Arctic lower troposphere. The efficiency of BC removal tends to be size‐independent during transport, leading to the observed similarity.Keywords
Funding Information
- Japan Society for the Promotion of Science (JP12J06736, JP1604452, JP16J04452, JP23221001, JP26241003, JP26701004, JP16H01770, JP17H04709, JP18H03363, JP18H05292, JP19K20441, JP20H00638, JP18H04140)
- Ministry of Education, Culture, Sports, Science and Technology
This publication has 92 references indexed in Scilit:
- Analysis of CCN activity of Arctic aerosol and Canadian biomass burning during summer 2008Atmospheric Chemistry and Physics, 2013
- Size dependence of wet removal of black carbon aerosols during transport from the boundary layer to the free troposphereGeophysical Research Letters, 2012
- How Well Are We Measuring Snow: The NOAA/FAA/NCAR Winter Precipitation Test BedBulletin of the American Meteorological Society, 2012
- Consistency and Traceability of Black Carbon Measurements Made by Laser-Induced Incandescence, Thermal-Optical Transmittance, and Filter-Based Photo-Absorption TechniquesAerosol Science and Technology, 2011
- Uncertainty assessment of current size-resolved parameterizations for below-cloud particle scavenging by rainAtmospheric Chemistry and Physics, 2010
- Source identification of short-lived air pollutants in the Arctic using statistical analysis of measurement data and particle dispersion model outputAtmospheric Chemistry and Physics, 2010
- Aerosol black carbon in the European Arctic: Measurements at Zeppelin station, Ny‐Ålesund, Svalbard from 1998–2007Geophysical Research Letters, 2009
- Arctic haze: current trends and knowledge gapsTellus B: Chemical and Physical Meteorology, 2007
- Full-Time, Eye-Safe Cloud and Aerosol Lidar Observation at Atmospheric Radiation Measurement Program Sites: Instruments and Data ProcessingJournal of Atmospheric and Oceanic Technology, 2002
- Arctic air pollution: An overview of current knowledgeAtmospheric Environment (1967), 1986