<?xml version="1.0" encoding="UTF-8"?><resource xsi:schemaLocation="http://datacite.org/schema/kernel-4 http://schema.datacite.org/meta/kernel-4.3/metadata.xsd" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns="http://datacite.org/schema/kernel-4"><identifier identifierType="DOI">10.1594/PANGAEA.965468</identifier><creators><creator><creatorName>Weller, Rolf</creatorName><givenName>Rolf</givenName><familyName>Weller</familyName><nameIdentifier schemeURI="http://orcid.org/" nameIdentifierScheme="ORCID">0000-0003-4880-5572</nameIdentifier><affiliation affiliationIdentifierScheme="ROR" affiliationIdentifier="https://ror.org/032e6b942">Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven</affiliation></creator></creators><titles><title>Aerosol light absorption coefficients and black carbon concentrations at Neumayer for the year 2023</title></titles><publisher>PANGAEA</publisher><publicationYear>2024</publicationYear><subjects><subject>aerosol</subject><subject>AIRCHEM</subject><subject>Atmospheric chemistry</subject><subject>Spuso</subject><subject subjectScheme="Parameter">HEIGHT above ground</subject><subject subjectScheme="Parameter">DATE/TIME</subject><subject subjectScheme="Parameter">Duration</subject><subject subjectScheme="Parameter">Aerosol absorption at 637 nm</subject><subject subjectScheme="Parameter">Black carbon, aerosol</subject><subject subjectScheme="Method">Air chemistry observatory</subject><subject subjectScheme="Method">Multi angle absorption spectrometer MAAP5012</subject><subject subjectScheme="Campaign">Neumayer_based</subject><subject subjectScheme="Basis">NEUMAYER III</subject><subject subjectScheme="Project">Atmospheric Chemistry @ AWI (AWI_AC)</subject></subjects><contributors><contributor contributorType="HostingInstitution"><contributorName>Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven</contributorName><nameIdentifier nameIdentifierScheme="ROR">https://ror.org/032e6b942</nameIdentifier></contributor></contributors><dates><date dateType="Collected">2023-01-01T00:00:00/2024-01-01T00:00:00</date></dates><resourceType resourceTypeGeneral="Dataset">Dataset</resourceType><relatedIdentifiers><relatedIdentifier relatedIdentifierType="DOI" relationType="IsPartOf">10.1594/PANGAEA.987702</relatedIdentifier><relatedIdentifier relatedIdentifierType="DOI" relationType="References">10.1594/PANGAEA.938991</relatedIdentifier><relatedIdentifier relatedIdentifierType="DOI" relationType="References">10.1594/PANGAEA.956089</relatedIdentifier><relatedIdentifier relatedIdentifierType="DOI" relationType="References">10.1594/PANGAEA.956056</relatedIdentifier></relatedIdentifiers><sizes><size>26274 data points</size></sizes><formats><format>text/tab-separated-values</format></formats><rightsList><rights rightsURI="https://creativecommons.org/licenses/by/4.0/" schemeURI="https://spdx.org/licenses/" rightsIdentifierScheme="SPDX" rightsIdentifier="CC-BY-4.0">Creative Commons Attribution 4.0 International</rights></rightsList><descriptions><description descriptionType="Abstract">We operate a multi angle absorption photometer MAAP (Model 5012, Thermo Electron Corp.). which is in operation since March 2006 ongoing. This instrument measures atmospheric light absorption by aerosol (mainly caused by black carbon, BC). To this end, ambient aerosol was sampled on a glass filter tape. The measured absorption coefficients abs(637) refer to a wavelength of 637 nm. Raw data were originally sampled in one-minute resolution. Finally, hourly averaged MAAP data are presented here. We also provide BC concentrations (ng/m³) derived from the absorption coefficients using the specific BC attenuation cross section (QBC) of 6.6 m²/g.</description><description descriptionType="TechnicalInfo">Important notice: BC concentrations are extremely low at Neumayer, typically lower than the instrumental noise level referring to 1 hour averages (between 0.04 and 0.05 Mm-1). Notwithstanding, we archived hourly averages, but one has to be aware that negative values may not be removed when smoothing the data or when calculating averages with lower temporal resolution, otherwise the results would exhibit a substantial positive bias!</description></descriptions><geoLocations><geoLocation><geoLocationPoint><pointLongitude>-8.25</pointLongitude><pointLatitude>-70.65</pointLatitude></geoLocationPoint></geoLocation><geoLocation><geoLocationPlace>Dronning Maud Land, Antarctica</geoLocationPlace></geoLocation></geoLocations></resource>