Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ...

Aerosol optical depth (AOD) is measured by a sun photometer, type SP1a by Dr. Schulz & Partner GmbH in 17 wavelengths between λ = 369nm to 1023nm with a field of view of 1° × 1° and a time resolution of 1 minute. In winter 2012/13 a new sun photometer was installed and just 10 of 17 wavelengths...

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Bibliographic Details
Main Authors: Graßl, Sandra, Ritter, Christoph
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2021
Subjects:
AOD
Online Access:https://dx.doi.org/10.1594/pangaea.937554
https://doi.pangaea.de/10.1594/PANGAEA.937554
id ftdatacite:10.1594/pangaea.937554
record_format openpolar
spelling ftdatacite:10.1594/pangaea.937554 2024-06-09T07:43:48+00:00 Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ... Graßl, Sandra Ritter, Christoph 2021 application/zip https://dx.doi.org/10.1594/pangaea.937554 https://doi.pangaea.de/10.1594/PANGAEA.937554 en eng PANGAEA https://dx.doi.org/10.3390/rs11111362 https://dx.doi.org/10.1594/pangaea.940018 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Angstrom Parameter AOD Arctic Arctic aerosol AWIPEV KOL03 Ny-Ålesund remote sensing Sun photometer Svalbard Research station AWIPEV_based Publication Series of Datasets article Collection 2021 ftdatacite https://doi.org/10.1594/pangaea.93755410.3390/rs1111136210.1594/pangaea.940018 2024-05-13T12:44:57Z Aerosol optical depth (AOD) is measured by a sun photometer, type SP1a by Dr. Schulz & Partner GmbH in 17 wavelengths between λ = 369nm to 1023nm with a field of view of 1° × 1° and a time resolution of 1 minute. In winter 2012/13 a new sun photometer was installed and just 10 of 17 wavelengths remained in the same wavelength range. With the nine out of ten wavelengths optical parameters like the AOD are computed. The one, which is devoted to water vapor is omitted. The instrument is calibrated regularly in pristine conditions at Izaña, Tenerife, via Langley method. A cloud screening based on short scale fluctuations of the AOD is used. The uncertainty for the AOD is generally said to be around 0.01. However, this is the maximum error of the instrument because the fluctuations are much smaller by comparing data minute by minute under low or constant aerosol conditions.The number of individual measurements differs between a few hundreds, especially in March and September, to up to 12,000 in early summer. ... Article in Journal/Newspaper Arctic Ny Ålesund Ny-Ålesund Svalbard DataCite Metadata Store (German National Library of Science and Technology) Arctic Ny-Ålesund Svalbard
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Angstrom Parameter
AOD
Arctic
Arctic aerosol
AWIPEV
KOL03
Ny-Ålesund
remote sensing
Sun photometer
Svalbard
Research station
AWIPEV_based
spellingShingle Angstrom Parameter
AOD
Arctic
Arctic aerosol
AWIPEV
KOL03
Ny-Ålesund
remote sensing
Sun photometer
Svalbard
Research station
AWIPEV_based
Graßl, Sandra
Ritter, Christoph
Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ...
topic_facet Angstrom Parameter
AOD
Arctic
Arctic aerosol
AWIPEV
KOL03
Ny-Ålesund
remote sensing
Sun photometer
Svalbard
Research station
AWIPEV_based
description Aerosol optical depth (AOD) is measured by a sun photometer, type SP1a by Dr. Schulz & Partner GmbH in 17 wavelengths between λ = 369nm to 1023nm with a field of view of 1° × 1° and a time resolution of 1 minute. In winter 2012/13 a new sun photometer was installed and just 10 of 17 wavelengths remained in the same wavelength range. With the nine out of ten wavelengths optical parameters like the AOD are computed. The one, which is devoted to water vapor is omitted. The instrument is calibrated regularly in pristine conditions at Izaña, Tenerife, via Langley method. A cloud screening based on short scale fluctuations of the AOD is used. The uncertainty for the AOD is generally said to be around 0.01. However, this is the maximum error of the instrument because the fluctuations are much smaller by comparing data minute by minute under low or constant aerosol conditions.The number of individual measurements differs between a few hundreds, especially in March and September, to up to 12,000 in early summer. ...
format Article in Journal/Newspaper
author Graßl, Sandra
Ritter, Christoph
author_facet Graßl, Sandra
Ritter, Christoph
author_sort Graßl, Sandra
title Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ...
title_short Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ...
title_full Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ...
title_fullStr Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ...
title_full_unstemmed Sun Photometer Data (AOD) from Ny-Ålesund, Svalbard (AWIPEV) ...
title_sort sun photometer data (aod) from ny-ålesund, svalbard (awipev) ...
publisher PANGAEA
publishDate 2021
url https://dx.doi.org/10.1594/pangaea.937554
https://doi.pangaea.de/10.1594/PANGAEA.937554
geographic Arctic
Ny-Ålesund
Svalbard
geographic_facet Arctic
Ny-Ålesund
Svalbard
genre Arctic
Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet Arctic
Ny Ålesund
Ny-Ålesund
Svalbard
op_relation https://dx.doi.org/10.3390/rs11111362
https://dx.doi.org/10.1594/pangaea.940018
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_doi https://doi.org/10.1594/pangaea.93755410.3390/rs1111136210.1594/pangaea.940018
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