Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New Zealand

Changes in stratospheric ozone have to be assessed continuously to evaluate the effectiveness of the Montreal Protocol. In the southern hemisphere, few ground-based observational datasets exist, making measurements at the Network for the Detection of Atmospheric Composition Change (NDACC) station at...

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Main Authors: Leonie Bernet, Ian Boyd, Gerald Nedoluha, Richard Querel, Daan Swart, Klemens Hocke
Format: Article
Language:English
Published: MDPI AG 2020-12-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/1/109
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author Leonie Bernet
Ian Boyd
Gerald Nedoluha
Richard Querel
Daan Swart
Klemens Hocke
author_facet Leonie Bernet
Ian Boyd
Gerald Nedoluha
Richard Querel
Daan Swart
Klemens Hocke
author_sort Leonie Bernet
collection DOAJ
description Changes in stratospheric ozone have to be assessed continuously to evaluate the effectiveness of the Montreal Protocol. In the southern hemisphere, few ground-based observational datasets exist, making measurements at the Network for the Detection of Atmospheric Composition Change (NDACC) station at Lauder, New Zealand invaluable. Investigating these datasets in detail is essential to derive realistic ozone trends. We compared lidar data and microwave radiometer data with collocated Aura Microwave Limb sounder (MLS) satellite data and ERA5 reanalysis data. The detailed comparison makes it possible to assess inhomogeneities in the data. We find good agreement between the datasets but also some possible biases, especially in the ERA5 data. The data uncertainties and the inhomogeneities were then considered when deriving trends. Using two regression models from the Long-term Ozone Trends and Uncertainties in the Stratosphere (LOTUS) project and from the Karlsruhe Institute of Technology (KIT), we estimated resulting ozone trends. Further, we assessed how trends are affected by data uncertainties and inhomogeneities. We find positive ozone trends throughout the stratosphere between 0% and 5% per decade and show that considering data uncertainties and inhomogeneities in the regression affects the resulting trends.
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spelling doaj.art-fa55be2361234138922f9b26f70d65d12023-11-21T07:27:51ZengMDPI AGRemote Sensing2072-42922020-12-0113110910.3390/rs13010109Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New ZealandLeonie Bernet0Ian Boyd1Gerald Nedoluha2Richard Querel3Daan Swart4Klemens Hocke5Institute of Applied Physics, University of Bern, 3012 Bern, SwitzerlandBC Scientific Consulting LLC, Stony Brook, NY 11790, USANaval Research Laboratory, Remote Sensing Division, Washington, DC 20375, USANational Institute of Water & Atmospheric Research, Lauder 9377, New ZealandNational Institute for Public Health and the Environment (RIVM), 3720 Bilthoven, The NetherlandsInstitute of Applied Physics, University of Bern, 3012 Bern, SwitzerlandChanges in stratospheric ozone have to be assessed continuously to evaluate the effectiveness of the Montreal Protocol. In the southern hemisphere, few ground-based observational datasets exist, making measurements at the Network for the Detection of Atmospheric Composition Change (NDACC) station at Lauder, New Zealand invaluable. Investigating these datasets in detail is essential to derive realistic ozone trends. We compared lidar data and microwave radiometer data with collocated Aura Microwave Limb sounder (MLS) satellite data and ERA5 reanalysis data. The detailed comparison makes it possible to assess inhomogeneities in the data. We find good agreement between the datasets but also some possible biases, especially in the ERA5 data. The data uncertainties and the inhomogeneities were then considered when deriving trends. Using two regression models from the Long-term Ozone Trends and Uncertainties in the Stratosphere (LOTUS) project and from the Karlsruhe Institute of Technology (KIT), we estimated resulting ozone trends. Further, we assessed how trends are affected by data uncertainties and inhomogeneities. We find positive ozone trends throughout the stratosphere between 0% and 5% per decade and show that considering data uncertainties and inhomogeneities in the regression affects the resulting trends.https://www.mdpi.com/2072-4292/13/1/109stratospheric ozonetrendsozone profilesmicrowave radiometrylidars
spellingShingle Leonie Bernet
Ian Boyd
Gerald Nedoluha
Richard Querel
Daan Swart
Klemens Hocke
Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New Zealand
Remote Sensing
stratospheric ozone
trends
ozone profiles
microwave radiometry
lidars
title Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New Zealand
title_full Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New Zealand
title_fullStr Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New Zealand
title_full_unstemmed Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New Zealand
title_short Validation and Trend Analysis of Stratospheric Ozone Data from Ground-Based Observations at Lauder, New Zealand
title_sort validation and trend analysis of stratospheric ozone data from ground based observations at lauder new zealand
topic stratospheric ozone
trends
ozone profiles
microwave radiometry
lidars
url https://www.mdpi.com/2072-4292/13/1/109
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