D. A. Degenstein

ORCID: 0000-0003-0358-2256
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About
Contact & Profiles
Research Areas
  • Atmospheric Ozone and Climate
  • Atmospheric and Environmental Gas Dynamics
  • Atmospheric chemistry and aerosols
  • Ionosphere and magnetosphere dynamics
  • Atmospheric aerosols and clouds
  • Calibration and Measurement Techniques
  • Air Quality Monitoring and Forecasting
  • Solar and Space Plasma Dynamics
  • Spectroscopy and Laser Applications
  • Climate variability and models
  • Astro and Planetary Science
  • Optical Imaging and Spectroscopy Techniques
  • Vehicle emissions and performance
  • Geophysics and Gravity Measurements
  • Planetary Science and Exploration
  • Meteorological Phenomena and Simulations
  • Water Quality Monitoring and Analysis
  • Cryospheric studies and observations
  • Methane Hydrates and Related Phenomena
  • Arctic and Antarctic ice dynamics
  • Aerospace Engineering and Energy Systems
  • Air Quality and Health Impacts
  • Gas Dynamics and Kinetic Theory
  • Solar Radiation and Photovoltaics
  • Geochemistry and Geologic Mapping

University of Saskatchewan
2016-2025

National Institute of Meteorology
2015

York University
2009-2011

National Research Council Canada
2010

Odin is a 250 kg class satellite built in co-operation between Sweden, Canada, France, and Finland launched February 2001. It carries two instruments: 4-band sub-millimetre radiometer used for both astronomy atmospheric science an optical spectrometer infrared imaging system purely observations. As part of the joint mission will observe limb 50% observation time producing profiles many species interest middle atmosphere with vertical resolution 1–2 km. These include, among others, ozone,...

10.1139/p01-157 article EN Canadian Journal of Physics 2002-03-01

The optical spectrograph and infrared imager system (OSIRIS) on board the Odin spacecraft is designed to retrieve altitude profiles of terrestrial atmospheric minor species by observing limb-radiance profiles. grating (OS) obtains spectra scattered sunlight over range 280–800 nm with a spectral resolution approximately 1 nm. performs repetitive vertical limb scan sweep OS km field view selected ranges from 10 100 km. absorption features that are superimposed solar spectrum monitored derive...

10.1139/p04-005 article EN Canadian Journal of Physics 2004-06-01

[1] The variability of stratospheric aerosol loading between 1985 and 2010 is explored with measurements from SAGE II, CALIPSO, GOMOS/ENVISAT, OSIRIS/Odin space-based instruments. We find that, following the 1991 eruption Mount Pinatubo, levels increased by as much two orders magnitude only reached "background levels" 1998 2002. From 2002 onwards, a systematic increase has been reported number investigators. Recently, trend, based on ground-based lidar measurements, tentatively attributed to...

10.1029/2011gl047563 article EN Geophysical Research Letters 2011-06-01

TROPOMI, on-board the Sentinel-5 Precursor satellite is a nadir-viewing spectrometer measuring reflected sunlight in ultraviolet, visible, near-infrared, and shortwave infrared spectral range. From these spectra several important air quality climate-related atmospheric constituents are retrieved at an unprecedented high spatial resolution, including nitrogen dioxide (NO2). We present first retrievals of TROPOMI NO2 over Canadian Oil Sands, contrasting them with observations from OMI...

10.1029/2018gl081095 article EN cc-by-nc-nd Geophysical Research Letters 2018-12-28

Abstract. Ozone forms in the Earth's atmosphere from photodissociation of molecular oxygen, primarily tropical stratosphere. It is then transported to extratropics by Brewer–Dobson circulation (BDC), forming a protective ozone layer around globe. Human emissions halogen-containing ozone-depleting substances (hODSs) led decline stratospheric until they were banned Montreal Protocol, and since 1998 upper stratosphere rising again, likely recovery halogen-induced losses. Total column...

10.5194/acp-18-1379-2018 article EN cc-by Atmospheric chemistry and physics 2018-02-06

Abstract. Ozone profile trends over the period 2000 to 2016 from several merged satellite ozone data sets and ground-based measured by four techniques at stations of Network for Detection Atmospheric Composition Change indicate significant increases in upper stratosphere, between 35 48 km altitude (5 1 hPa). Near 2 hPa (42 km), has been increasing about 1.5 % per decade tropics (20° S 20° N), 2.5 60° latitude bands both hemispheres. At levels below hPa), are smaller not statistically...

10.5194/acp-17-10675-2017 article EN cc-by Atmospheric chemistry and physics 2017-09-11

SignificanceLarge wildfires have been observed to inject smoke into the stratosphere, raising questions about their potential affect stratospheric ozone layer that protects life on Earth from biologically damaging ultraviolet radiation. Multiple observations of aerosol and NO2 concentrations three independent satellite instruments are used here together with model calculations identify decreases in following major Australian 2019 through 2020 wildfires. The data confirm important chemistry...

10.1073/pnas.2117325119 article EN cc-by Proceedings of the National Academy of Sciences 2022-03-01

In June 2009 the Sarychev volcano located in Kuril Islands to northeast of Japan erupted explosively, injecting ash and an estimated 1.2 ± 0.2 Tg sulfur dioxide into upper troposphere lower stratosphere, making it arguably one 10 largest stratospheric injections last 50 years. During period immediately after eruption, we show that (SO 2 ) cloud was clearly detected by retrievals developed for Infrared Atmospheric Sounding Interferometer (IASI) satellite instrument resultant sulfate aerosol...

10.1029/2010jd014447 article EN Journal of Geophysical Research Atmospheres 2010-11-12

Abstract. Trends in the vertical distribution of ozone are reported and compared for a number new recently revised data sets. The amount ozone-depleting compounds stratosphere (as measured by equivalent effective stratospheric chlorine – EESC) was maximised second half 1990s. We examine periods before after peak to see if any change trend is discernible record that might be attributable EESC trend, though no attribution attempted. Prior 1998, trends upper (~ 45 km, 4 hPa) found −5 −10 % per...

10.5194/acp-15-9965-2015 article EN cc-by Atmospheric chemistry and physics 2015-09-07

Abstract. This paper presents extensive {bias determination} analyses of ozone observations from the Atmospheric Chemistry Experiment (ACE) satellite instruments: ACE Fourier Transform Spectrometer (ACE-FTS) and Measurement Aerosol Extinction in Stratosphere Troposphere Retrieved by Occultation (ACE-MAESTRO) instrument. Here we compare latest data products ACE-FTS ACE-MAESTRO with coincident nearly 20 satellite-borne, airborne, balloon-borne ground-based instruments, analysing volume mixing...

10.5194/acp-9-287-2009 article EN cc-by Atmospheric chemistry and physics 2009-01-16

Abstract. The ozone profile records of a large number limb and occultation satellite instruments are widely used to address several key questions in research. Further progress some domains depends on more detailed understanding these data sets, especially their long-term stability mutual consistency. To this end, we made systematic assessment 14 sounders that, together, provide than three decades global measurements. In particular, considered the latest operational Level-2 by SAGE II, III,...

10.5194/amt-9-2497-2016 article EN cc-by Atmospheric measurement techniques 2016-06-08

Abstract The Optical Spectrograph and InfraRed Imaging System (OSIRIS) on board the Odin satellite has been used to provide vertically resolved aerosol extinction since 2001. OSIRIS version 5.07 product in numerous studies now provides a 17‐year record of global stratospheric aerosol. This work presents new 7 retrieval. A multiwavelength algorithm developed reduce measurement geometry biases improve retrieval upper troposphere lower stratosphere. Chen et al. (2016,...

10.1029/2018jd029897 article EN Journal of Geophysical Research Atmospheres 2019-06-14

The cover shows a cropped image of the warming stripes (seen in full below), as developed by Ed Hawkins (Reading University, UK).Each vertical line global average temperature whole year, starting at 1850 on far left and ending with 2019 right.The underlying data are from HadCRUT4.6dataset UK Met Office Hadley Centre.To create other regions countries visit https://showyourstripes.

10.1175/bams-d-20-0104.1 article EN Bulletin of the American Meteorological Society 2020-08-01

Abstract The Stratospheric Aerosol and Gas Experiment III on the International Space Station (SAGE III/ISS) was launched 19 February 2017 began routine operation in June 2017. first 2 years of SAGE III/ISS (v5.1) solar occultation ozone data were evaluated by using correlative satellite ground‐based measurements. Among three (MES, AO3, MLR) retrieved products, AO3 shows smallest bias best precision, with mean biases less than 5% for altitudes ~15–55 km midlatitudes ~20–55 tropics. In lower...

10.1029/2020jd032430 article EN cc-by Journal of Geophysical Research Atmospheres 2020-05-16
Robert Dunn Freya Aldred Nadine Gobron J. B. Miller Kate M. Willett and 95 more Melanie Ades Robert F. Adler Richard P. Allan Rob Allan J. G. Anderson Anthony Argüez Carlo Arosio John Augustine César Azorín-Molina Jonathan Barichivich Hylke E. Beck Andreas Becker Nicolas Bellouin Angela Benedetti David I. Berry Stephen Blenkinsop Olivier Bock Xavier Bodin Michael G. Bosilovich Oliviér Boucher Stefan A. Buehler Beatriz Calmettes Laura Carrea Laura Castia Hanne H. Christiansen John R. Christy Eui‐Seok Chung Melanie Coldewey‐Egbers O. R. Cooper Richard Cornes Curt Covey J.-F. Crétaux Molly Crotwell Sean Davis Richard de Jeu D. A. Degenstein Reynald Delaloye Larry Di Girolamo Markus G. Donat Wouter Dorigo Imke Durre G. S. Dutton Grégory Duveiller J. W. Elkins Vitali Fioletov Johannes Flemming Michael J. Foster S. M. Frith Lucien Froidevaux Judith Garforth Matthew Gentry S. K. Gupta Sebastian Hahn Leopold Haimberger B. D. Hall Ian Harris Debbie Hemming Martin Hirschi Shu-pen Ho Filip Hrbáček Daan Hubert D. F. Hurst Antje Inness Ketil Isaksen Viju O. John P. D. Jones Robert Junod Johannes W. Kaiser Viktor Kaufmann Andreas Kellerer‐Pirklbauer Elizabeth C. Kent Robert B. Kidd Hyungjun Kim Zak Kipling Akash Koppa Benjamin M. Kraemer David P. Kratz Xin Lan Kathleen Lantz David A. Lavers Norman G. Loeb Diego Loyola Rémi Madelon Michael Mayer Matthew F. McCabe Tim R. McVicar C. A. Mears Christopher J. Merchant Diego G. Miralles Leander Moesinger S. A. Montzka Colin Morice Leander Mösinger Jens Mühle Julien P. Nicolas

10.1175/bams-d-21-0098.1 article Bulletin of the American Meteorological Society 2021-08-01

Abstract. After decades of depletion in the 20th century, near-global ozone now shows clear signs recovery upper stratosphere. The column, however, has remained largely constant since turn mainly due to evolution lower stratospheric ozone. In tropical stratosphere, is expected decrease as a consequence enhanced upwelling driven by increasing greenhouse gas concentrations, and this consistent with observations. There recent evidence, that mid-latitude continues well, contrary model...

10.5194/acp-22-9553-2022 article EN cc-by Atmospheric chemistry and physics 2022-07-25
Robert Dunn Freya Aldred Nadine Gobron J. B. Miller Kate M. Willett and 95 more Melanie Ades Robert E. Adler Richard P. Allan John C. Anderson Orlane Anneville Yasuyuki Aono Anthony Argüez Carlo Arosio John Augustine César Azorín-Molina Jonathan Barichivich Aman Basu Hylke E. Beck Nicolas Bellouin Angela Benedetti Kevin Blagrave Stephen Blenkinsop Olivier Bock Xavier Bodin Michael G. Bosilovich Oliviér Boucher Gerald Bové Dennis E. Buechler Stefan A. Buehler Laura Carrea Kai‐Lan Chang Hanne H. Christiansen John R. Christy Eui‐Seok Chung Laura M. Ciasto Melanie Coldewey‐Egbers O. R. Cooper Richard Cornes Curt Covey Thomas Cropper Molly Crotwell Diego Cusicanqui Sean Davis Richard de Jeu D. A. Degenstein Reynald Delaloye Markus G. Donat Wouter Dorigo Imke Durre G. S. Dutton Grégory Duveiller J. W. Elkins T. W. Estilow Nava Fedaeff David Fereday Vitali Fioletov Johannes Flemming Michael J. Foster S. M. Frith Lucien Froidevaux Martin Füllekrug Judith Garforth Jay Garg Matthew Gentry Steven M. Goodman Qiqi Gou Nikolay Granin Mauro Guglielmin Sebastian Hahn Leopold Haimberger B. D. Hall Ian Harris Debbie Hemming Martin Hirschi Shu-pen Ho R. H. Holzworth Filip Hrbáček Daan Hubert Petra Hulsman D. F. Hurst Antje Inness Ketil Isaksen Viju O. John P. D. Jones Robert Junod Andreas Kääb Johannes W. Kaiser Viktor Kaufmann Andreas Kellerer‐Pirklbauer Elizabeth C. Kent Richard Kidd Hyungiun Kim Zak Kipling Akash Koppa Jan Henning L'Abée‐Lund Xin Lan Kathleen Lantz David A. Lavers Norman G. Loeb Diego Loyola

Caption: Lightning discharges appear in various colours depending on the scatter of light inside thundercloud and atmosphere.The intracloud lightning centre to be white with a bluish tint, cloud-to-ground discharge below appears orange.The right hand side exhibits green tint that is attributed unique composition hydrometeors thundercloud.The photo was taken late evening 10 September 2013, near Tarragona northeastern Spain.

10.1175/bams-d-22-0092.1 article EN Bulletin of the American Meteorological Society 2022-08-01

Abstract. This study presents an updated evaluation of stratospheric ozone profile trends in the 60∘ S–60∘ N latitude range over 2000–2020 period using version Long-term Ozone Trends and Uncertainties Stratosphere (LOTUS) regression model that was used to evaluate such up 2016 for last WMO Assessment (2018). In addition derivation detailed as a function vertical coordinates, regressions are performed with datasets averaged broad bands, i.e. 60–35∘ S, 20∘ S–20∘ 35–60∘ N. The same methodology...

10.5194/acp-22-11657-2022 article EN cc-by Atmospheric chemistry and physics 2022-09-09

Abstract The 2022 eruption of the Hunga Tonga‐Hunga Ha'apai volcano caused substantial impacts on atmosphere, including a massive injection water vapor, and largest increase in stratospheric aerosol for 30 years. Ozone Mapping Profiler Suite (OMPS) Limb instrument has been critical monitoring amount spread volcanic stratosphere. We show that rapid imagery from OMPS enables tomographic retrieval extinction reduces bias up to factor two, improves vertical structure agreement with coincident...

10.1029/2022gl101978 article EN cc-by-nc Geophysical Research Letters 2023-02-01
Robert Dunn J. B. Miller Kate M. Willett Nadine Gobron Melanie Ades and 95 more Robert F. Adler Mihai Alexe Richard P. Allan John C. Anderson Orlane Anneville Yasuyuki Aono Anthony Argüez Carlo Arosio John Augustine César Azorín-Molina Jonathan Barichivich John Barnes Hylke E. Beck Nicolas Bellouin Angela Benedetti Kevin Blagrave Stephen Blenkinsop Olivier Bock Xavier Bodin Michael G. Bosilovich Oliviér Boucher Dennis E. Buechler Stefan A. Buehler Diego Campos Laura Carrea Kai‐Lan Chang Hanne H. Christiansen John R. Christy Eui‐Seok Chung Laura M. Ciasto Scott Clingan Melanie Coldewey‐Egbers O. R. Cooper Richard Cornes Curt Covey Jean-François Créatux Theresa M. Crimmins Thomas Cropper Molly Crotwell Joshua Culpepper Diego Cusicanqui Sean Davis Richard de Jeu D. A. Degenstein Reynald Delaloye Martin T. Dokulil Markus G. Donat Wouter Dorigo Hilary A. Dugan Imke Durre G. S. Dutton Grégory Duveiller T. W. Estilow Nicole Estrella David Fereday Vitali Fioletov Johannes Flemming Michael J. Foster Bryan A. Franz S. M. Frith Lucien Froidevaux Martin Füllekrug Judith Garforth Jay Garg Badin Gibbes Steven M. Goodman Atsushi Goto A. Gruber Guojun Gu Sebastian Hahn Leopold Haimberger B. D. Hall Ian Harris Deborah Hemming Martin Hirschi Shu‐peng Ho R. H. Holzworth Filip Hrbáček Guojie Hu D. F. Hurst Antje Inness Ketil Isaksen Viju O. John P. D. Jones Robert Junod Andreas Kääb Johannes W. Kaiser Viktor Kaufmann Andreas Kellerer‐Pirklbauer Elizabeth C. Kent Richard Kidd Zak Kipling Akash Koppa Benjamin M. Kraemer N. A. Kramarova

© 2023 American Meteorological Society. For information regarding reuse of this content and general copyright information, consult the AMS Copyright Policy (www.ametsoc.org/PUBSReuseLicenses). Corresponding author: Robert Dunn / robert.dunn@metoffice.gov.uk

10.1175/bams-d-23-0090.1 article EN cc-by Bulletin of the American Meteorological Society 2023-09-01

An algorithm for the retrieval of global stratospheric aerosol profiles is presented using optical spectrograph and infrared imaging system limb scatter measurements as an example data set. The utilizes a one‐dimensional version MART nonlinear relaxation inversion suitable scatter. A height profile particle size distribution must be assumed in order to retrieve number density. altitude normalized wavelength ratio measurement vector employed minimize effects upwelling radiation from ground...

10.1029/2006jd008079 article EN Journal of Geophysical Research Atmospheres 2007-05-24

In September 2002 the Antarctic polar vortex split in two under influence of a sudden warming. During this event, Odin satellite was able to measure both ozone (O 3 ) and chlorine monoxide (ClO), key constituent responsible for so‐called “ozone hole”, together with nitrous oxide (N 2 O), dynamical tracer, nitric acid (HNO nitrogen dioxide (NO ), tracers denitrification. The submillimeter radiometer (SMR) microwave instrument Optical Spectrograph Infrared Imager System (OSIRIS) UV‐visible...

10.1029/2004jd005018 article EN Journal of Geophysical Research Atmospheres 2005-03-11

Abstract. The OSIRIS instrument onboard the Odin spacecraft routinely measures vertical profiles of spectrally dispersed, limb scattered sunlight from upper troposphere into lower mesosphere. These measurements are used to retrieve ozone number density profile using SaskMART Multiplicative Algebraic Reconstruction Technique, which is a one dimensional modification an existing two-dimensional tomographic retrieval algorithm. retrieved extends cloud top 60 km. In absence clouds down 10 This...

10.5194/acp-9-6521-2009 article EN cc-by Atmospheric chemistry and physics 2009-09-09
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