Mikalai Filonchyk , Michael P. Peterson , Volha Hurynovich , Lifeng Zhang , Yi He
{"title":"Aerosol composition and properties in Antarctica: Optical, microphysical, and radiative characteristics","authors":"Mikalai Filonchyk , Michael P. Peterson , Volha Hurynovich , Lifeng Zhang , Yi He","doi":"10.1016/j.gloplacha.2025.104935","DOIUrl":null,"url":null,"abstract":"<div><div>Antarctica's unique climate and pristine environment make it a critical region for understanding the role of aerosols in global climate change. This study utilizes data from the AERONET (Aerosol Robotic Network) and MERRA-2 (Modern-Era Retrospective Analysis for Research and Applications) reanalysis system to investigate the optical, microphysical, and radiative properties of aerosols in the Antarctic atmosphere. Data from seven AERONET stations across Antarctica are analyzed to provide insights into aerosol optical depth (AOD), aerosol volume size distribution (VSD), and direct aerosol radiative forcing (DARF). The study's findings indicate that the primary sources of aerosols in Antarctica are natural, such as sea salt from ocean spray and sulfates from marine phytoplankton. The AOD values at a wavelength of 500 nm range from 0.027 ± 0.019 to 0.082 ± 0.042, have the lowest values at inland sites and the highest at coastal sites like Escudero_Station. Fine-mode aerosols dominate across most sites, with peaks in the volume size distribution between 0.09 and 0.76 μm, which is clearly associated with stable meteorological dynamics. The study also examines the radiative properties of aerosols, finding that DARF at the bottom of the atmosphere (BOA) indicates a cooling effect, with negative values ranging from −14.3 ± 4 to −3 ± 0.5 W/m<sup>2</sup>. DARF at the top of the atmosphere (TOA) varies, with both positive and negative values, indicating the complex role of aerosols in the Antarctic climate. The atmospheric heating rate (HR), a measure of the impact of aerosols on temperature, showed variations across AERONET sites and seasons, with averages ranging from 0.03 ± 0.005 K day<sup>−1</sup> to 0.25 ± 0.03 K day<sup>−1</sup>. These results highlight Antarctica's significance in studying the impact on aerosols on climate processes. Despite low aerosol concentrations compared to other world regions, Antarctica's unique environmental conditions provide valuable insights into climate change mechanisms. The study underscores the need for further research to understand aerosol properties, sources, and their broader impact on global climate.</div></div>","PeriodicalId":55089,"journal":{"name":"Global and Planetary Change","volume":"253 ","pages":"Article 104935"},"PeriodicalIF":4.0000,"publicationDate":"2025-06-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Global and Planetary Change","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0921818125002449","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 0
Abstract
Antarctica's unique climate and pristine environment make it a critical region for understanding the role of aerosols in global climate change. This study utilizes data from the AERONET (Aerosol Robotic Network) and MERRA-2 (Modern-Era Retrospective Analysis for Research and Applications) reanalysis system to investigate the optical, microphysical, and radiative properties of aerosols in the Antarctic atmosphere. Data from seven AERONET stations across Antarctica are analyzed to provide insights into aerosol optical depth (AOD), aerosol volume size distribution (VSD), and direct aerosol radiative forcing (DARF). The study's findings indicate that the primary sources of aerosols in Antarctica are natural, such as sea salt from ocean spray and sulfates from marine phytoplankton. The AOD values at a wavelength of 500 nm range from 0.027 ± 0.019 to 0.082 ± 0.042, have the lowest values at inland sites and the highest at coastal sites like Escudero_Station. Fine-mode aerosols dominate across most sites, with peaks in the volume size distribution between 0.09 and 0.76 μm, which is clearly associated with stable meteorological dynamics. The study also examines the radiative properties of aerosols, finding that DARF at the bottom of the atmosphere (BOA) indicates a cooling effect, with negative values ranging from −14.3 ± 4 to −3 ± 0.5 W/m2. DARF at the top of the atmosphere (TOA) varies, with both positive and negative values, indicating the complex role of aerosols in the Antarctic climate. The atmospheric heating rate (HR), a measure of the impact of aerosols on temperature, showed variations across AERONET sites and seasons, with averages ranging from 0.03 ± 0.005 K day−1 to 0.25 ± 0.03 K day−1. These results highlight Antarctica's significance in studying the impact on aerosols on climate processes. Despite low aerosol concentrations compared to other world regions, Antarctica's unique environmental conditions provide valuable insights into climate change mechanisms. The study underscores the need for further research to understand aerosol properties, sources, and their broader impact on global climate.
期刊介绍:
The objective of the journal Global and Planetary Change is to provide a multi-disciplinary overview of the processes taking place in the Earth System and involved in planetary change over time. The journal focuses on records of the past and current state of the earth system, and future scenarios , and their link to global environmental change. Regional or process-oriented studies are welcome if they discuss global implications. Topics include, but are not limited to, changes in the dynamics and composition of the atmosphere, oceans and cryosphere, as well as climate change, sea level variation, observations/modelling of Earth processes from deep to (near-)surface and their coupling, global ecology, biogeography and the resilience/thresholds in ecosystems.
Key criteria for the consideration of manuscripts are (a) the relevance for the global scientific community and/or (b) the wider implications for global scale problems, preferably combined with (c) having a significance beyond a single discipline. A clear focus on key processes associated with planetary scale change is strongly encouraged.
Manuscripts can be submitted as either research contributions or as a review article. Every effort should be made towards the presentation of research outcomes in an understandable way for a broad readership.