Zobrazeno 1 - 10
of 31
pro vyhledávání: '"D. A. Newnham"'
Publikováno v:
Atmospheric Measurement Techniques, Vol 15, Pp 2361-2376 (2022)
Ground-based observations of 11.072 GHz atmospheric ozone (O3) emission have been made using the Ny-Ålesund Ozone in the Mesosphere Instrument (NAOMI) at the UK Arctic Research Station (latitude 78∘55′0′′ N, longitude 11∘55′59′′ E),
Externí odkaz:
https://doaj.org/article/025cab92bec8459ba73c7bc00696fac5
Publikováno v:
Atmospheric Measurement Techniques, Vol 12, Pp 1375-1392 (2019)
The Ku-band microwave frequencies (10.70–14.25 GHz) overlap emissions from ozone (O3) at 11.072 GHz and hydroxyl radical (OH) at 13.441 GHz. These important chemical species in the polar middle atmosphere respond strongly to high-latitude geo
Externí odkaz:
https://doaj.org/article/582ff94e777c464084b72a813e41be3d
Publikováno v:
Atmospheric Measurement Techniques, Vol 9, Pp 5461-5485 (2016)
The submillimetre is an understudied region of the Earth's atmospheric electromagnetic spectrum. Prior technological gaps and relatively high opacity due to the prevalence of rotational water vapour lines at these wavelengths have slowed progress
Externí odkaz:
https://doaj.org/article/860fa0a27afa467f870f431c638c35a4
Autor:
T. Kovács, J. M. C. Plane, W. Feng, T. Nagy, M. P. Chipperfield, P. T. Verronen, M. E. Andersson, D. A. Newnham, M. A. Clilverd, D. R. Marsh
Publikováno v:
Geoscientific Model Development, Vol 9, Iss 9, Pp 3123-3136 (2016)
This study presents a new ion–neutral chemical model coupled into the Whole Atmosphere Community Climate Model (WACCM). The ionospheric D-region (altitudes ∼ 50–90 km) chemistry is based on the Sodankylä Ion Chemistry (SIC) model, a one-dimens
Externí odkaz:
https://doaj.org/article/b01c0cea9ffb4b639136c5000dcf551a
Publikováno v:
Atmospheric Measurement Techniques, Vol 9, Iss 7, Pp 3309-3323 (2016)
Meteorological and atmospheric models are being extended up to 80 km altitude but there are very few observing techniques that can measure stratospheric–mesospheric winds at altitudes between 20 and 80 km to verify model datasets. Here we demonstra
Externí odkaz:
https://doaj.org/article/5132cd6a96ba486cb7dafaed64331413
Publikováno v:
Earth System Science Data, Vol 6, Iss 1, Pp 105-115 (2014)
This paper describes the stratospheric and mesospheric ozone profiles retrieved from spectral measurements of the 249.96 GHz O3 line, using the British Antarctic Survey's ground-based Microwave Radiometer at Troll (BAS-MRT), Antarctica (72°01' S, 02
Externí odkaz:
https://doaj.org/article/767a496a9f654de78d4f7f187d05c2aa
Publikováno v:
Earth System Science Data, Vol 5, Iss 1, Pp 199-208 (2013)
This paper presents mesospheric carbon monoxide (CO) data acquired by the ground-based microwave radiometer of the British Antarctic Survey (BAS radiometer) stationed at Troll station in Antarctica (72° S, 2.5° E, 1270 m a.s.l.). The dataset covers
Externí odkaz:
https://doaj.org/article/3aa0404f75054914b8ed5b154c0290be
Publikováno v:
Atmospheric Chemistry and Physics, Vol 5, Iss 1, Pp 47-56 (2005)
Absorption spectra of peroxyacetyl nitrate (PAN, CH3C(O)OONO2) vapour at room temperature (295K) have been measured in the mid-infrared range, 550-2200cm-1 (18.2-4.55µm), using a Fourier Transform infrared spectrometer at instrument resolutions of 0
Externí odkaz:
https://doaj.org/article/a35af0e1b9fd4499866068b95c4b403b
Publikováno v:
Earth System Science Data, Vol 5, Iss 1, Pp 199-208 (2013)
Earth System Science Data
Earth System Science Data
This paper presents mesospheric carbon monoxide (CO) data acquired by the ground-based microwave radiometer of the British Antarctic Survey (BAS radiometer) stationed at Troll station in Antarctica (72° S, 2.5° E, 1270 m a.s.l.). The dataset covers
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::345bd79e15917aa96b9e287266f3598b
https://www.earth-syst-sci-data.net/5/199/2013/
https://www.earth-syst-sci-data.net/5/199/2013/
Publikováno v:
Scopus-Elsevier
Measurements of BrO in the atmosphere are now routinely made using UV absorption spectroscopy, but it has recently been noted that the retrieved BrO amounts are critically dependent on the wavelength dependence of the ozone absorption cross sections