Reid S.J., G. Vaughan, A.R. Marsh, and H.G.J. Smit, Intercomparison
of ozone measurements by ECC sondes and BENDIX chemiluminescent analyser, J. Atm.
``... very little feedback came through to us until a telephone call from the United States embassy to say that Bob Watson was coming across, bringing some satellite pictures of the TOMS maps
of ozone measurements, would I like to wander down to the embassy to have a look at them....»
Not exact matches
Its core competence is the in - line
measurement of conductivity, resistivity, TOC, dissolved oxygen, bioburden, sodium, silica, chloride / sulphate and
ozone in determining and controlling water purity.
THORNTON is a leader for pure water treatment
measurement & control in pharmaceutical, semiconductor and power industries with parameters
of conductivity / resistivity, TOC, pH, DO, dissolved
ozone and flow.
Among them were the
measurements of atmospheric
ozone at the UK's Halley research station in Antarctica.
Robert Watson, a government official and co-chair
of the scientific panel that advises the Montreal Protocol, said that laboratory experiments, computer models, and field
measurements all support the conclusion that CFCs are destroying stratospheric
ozone.
From then on, scientists worldwide typically tracked
ozone depletion using October
measurements of Antarctic
ozone.
They analyzed
ozone measurements taken from weather balloons and satellites, as well as satellite
measurements of sulfur dioxide emitted by volcanoes, which can also enhance
ozone depletion.
They then compared their yearly September
ozone measurements with model simulations that predict
ozone levels based on the amount
of chlorine that scientists have estimated to be present in the atmosphere from year to year.
NOAA
measurements at South Pole station monitor the
ozone layer above that location by means
of Dobson spectrophotometer and regular
ozone - sonde balloon launches that record the thickness
of the
ozone layer and its vertical distribution.
Although the distribution
of these emissions is still uncertain,
measurements have indicated that the tropical oceans could be major sources, lofting them into the atmosphere where they can ultimately contribute to reactions that control tropospheric and stratospheric
ozone.
Even in the past
measurements from the peripheral sections
of the now investigated region showed minimal
ozone values in the area
of the upper troposphere, but not the consistently low values that have now been found across the entire depth
of the troposphere.
The
ozone concentrations in his
measurements remained nearly constantly below the detection limit
of approx. 10 ppbv in the entire vertical range from the surface
of Earth to an altitude
of around 15 kilometres.
Although low values at an altitude
of around 15 kilometres were known from earlier
measurements in the peripheral area
of the tropical West Pacific, the complete absence
of ozone at all heights was surprising.
There is also a considerable gap in the otherwise dense network
of global
ozone measurement stations here.
The researchers compared results from a model called GFDL - AM3 to
ozone measurements from monitoring stations over the course
of the last 35 years, from 1980 to 2014.
The WMO reports the lowest ever
measurements of Antarctic stratospheric
ozone — 105 Dobson units — from the South Pole a few weeks ago.
Researchers are currently making these
measurements using the Limb Profiler instrument, part
of Ozone Mapping Profiler Suite (OMPS) instrument, currently flying on the joint NASA / National Oceanic and Atmospheric Administration (NOAA)-RRB- / Department
of Defense Suomi National Polar - orbiting Partnership (Suomi NPP) satellite, launched in October 2011.
This possibility is set in a disturbing context by the latest
measurements of stratospheric
ozone by the World Meteorological Organization.
In August a study conducted by the Cooperative Institute for Research in Environmental Sciences in Colorado revealed that
ozone measurements have stopped declining over the midlatitudes
of the Northern and Southern hemispheres, where the bulk
of the world's population resides.
The
ozone measurements, taken between 2 and 6 miles in altitude (3 - 10 kilometers) over a large part
of the eastern Indian Ocean, were as high as 80 parts per billion - levels similar to a polluted day in a U.S. city and several times more than normal.
«This is the only long - term data set with regular
measurements of ozone - destroying compounds in the stratosphere,» says atmospheric chemist Darin Toohey
of the University
of California, Irvine.
Furthermore, other
measurement and model studies comparing the response
of mid-range vs. high
ozone values show that the
ozone decreases in the US and Europe are more pronounced for the highest
ozone values, while sites in China show
ozone increases for both mid-range and high
ozone values (Derwent et al., 2010; Simon et al., 2015; Lefohn et al., 2017b).
The
ozone measurements are really good, because the data our instrument collects contribute to creating maps
of ozone cover over Antarctica.
Answer to # 10:
Ozone values are *** VERY *** variable: even if there is a mean sinusoidal pattern over Europes latitudes (see http://www.meteo.be/english/pages/OzonEN.html or http://meteo.lcd.lu/dobson05.html) the variations from that mean trend are exceptional great: as such a local
measurement of low values is never a hint to a lowering trend (and the opposite is true also...).
Ozone measurements from the first week of March already show a region over the North Atlantic with very low ozone levels (< 250 Dobson units, versus minimum values of ~ 300 in the early 19
Ozone measurements from the first week
of March already show a region over the North Atlantic with very low
ozone levels (< 250 Dobson units, versus minimum values of ~ 300 in the early 19
ozone levels (< 250 Dobson units, versus minimum values
of ~ 300 in the early 1980s).
In Utqiagvik, Alaska (formerly known as Barrow)-- one
of a handful
of stations where NOAA measures Arctic
ozone levels — there's been a 12 percent increase in average
ozone levels since
measurement began 45 years ago, Cooper said.
Has realclimate ever done (or considered doing) an entry about the immense contribution that satellite
measurements have made in the past two - three decades, in helping us to understand various components
of the earth system (e.g., vegetation,
ozone, ice sheet mass, water vapor content, temperature, sea level height, storms, aerosols, etc.)?
Because even by tweaking things to be most generous, about 1/3
of the heating change can be made to fit the «no human CO2» scenario without putting something OBVIOUSLY wrong in there (like, say, trees outputting 100x the
ozone we see in
measurements today).
... This brings up the nightmarish thought that if the chemical industry had developed organobromine compounds instead
of the CFCs — or alternatively, if chlorine chemistry would have run more like that
of bromine — then without any preparedness, we would have been faced with a catastrophic
ozone hole everywhere and at all seasons during the 1970s, probably before the atmospheric chemists had developed the necessary knowledge to identify the problem and the appropriate techniques for the necessary critical
measurements.
Ozone measurements from the first week of March already show a region over the North Atlantic with very low ozone levels (< 250 Dobson units, versus minimum values of ~ 300 in the early 19
Ozone measurements from the first week
of March already show a region over the North Atlantic with very low
ozone levels (< 250 Dobson units, versus minimum values of ~ 300 in the early 19
ozone levels (< 250 Dobson units, versus minimum values
of ~ 300 in the early 1980s).
Their
measurements, focusing on a time period in September each year — during which time the colder temperatures in the atmosphere promote the reactions that destroy
ozone so that the hole is opening up — show that since 2000, the hole has shrunk by 1.7 million square miles, an area more than half the size
of the continental United States.
Answer to # 10:
Ozone values are *** VERY *** variable: even if there is a mean sinusoidal pattern over Europes latitudes (see http://www.meteo.be/english/pages/OzonEN.html or http://meteo.lcd.lu/dobson05.html) the variations from that mean trend are exceptional great: as such a local
measurement of low values is never a hint to a lowering trend (and the opposite is true also...).
NPP will continue
measurements of land surface vegetation, sea surface temperature, and atmospheric
ozone that began more than 25 years ago.
Ozone amounts in the depletion layer are the lowest seen in the 21 year record of ozone profile measurements at the South
Ozone amounts in the depletion layer are the lowest seen in the 21 year record
of ozone profile measurements at the South
ozone profile
measurements at the South Pole.
Heue, K. - P., Coldewey - Egbers, M., Delcloo, A., Lerot, C., Loyola, D., Valks, P., and van Roozendael, M.: Trends
of tropical tropospheric
ozone from 20 years
of European satellite
measurements and perspectives for the Sentinel - 5 Precursor, Atmos.
ACCMIP will take advantage
of these
measurements by performing extensive evaluations
of the models, especially as regards their simulations
of tropospheric
ozone and aerosols, both
of which have substantial climate forcing that varies widely in space and time.
This method uses consistency between direct normal and diffuse horizontal
measurements together with a special regression technique for retrieval
of daily time series
of column mean aerosol particle size, aerosol optical depth, NO2,
ozone and water vapor column amounts together with the instrument's calibration constants.
Measurements show that depletion
of the
ozone layer steadily worsened during the 1980s and most
of the 1990s, but more recently as atmospheric amounts
of chlorine and bromine have stabilized, a further worsening
of ozone depletion appears to have been avoided.
The error
of individual total
ozone measurements for a well maintained Brewer instrument is about 1 % (e.g. Kerr, 1988).
The error bar on ECV total
ozone data (δTOC) shall be assessed and expressed as the percent relative difference with respect to correlative
measurements of reference.
The dependence
of the ECV data quality on main
measurement and retrieval parameters like the solar zenith angle,
ozone column amount, latitude, and cloud parameters (fractional cloud cover, cloud top height and albedo, etc. as appropriate) shall be investigated.
The second factor is the insulating effect
of the atmosphere
of which well over 90 % results from atmospheric water in the form
of clouds and water vapour with the remaining 10 % due primarily from CO2 and
ozone with just a slightly detectable effect from methane and a trivial effect from all the other gases named in tyhe Kyoto Accord that is so small it can't even be detected on
measurements of the Earth's radiative spectrum.
Dobson
measurements suffer from a temperature dependence
of the
ozone absorption coefficients used in the retrievals which might account for a seasonal variation in the error
of ± 0.9 % in the middle latitudes and ± 1.7 % in the Arctic, and for systematic errors
of up to 4 % [Bernhard et al., 2005].
Randall et al. [1998, 2001] presented evidence from the Polar
Ozone and Aerosol
Measurement (POAM) II and III instruments for stratospheric O3 reductions caused by the EPP IE, showing depletions
of 40 — 45 % in middle stratospheric O3 mixing ratios.
Needed
measurements include not only the conventional climatic variables (temperature and precipitation), but also the time - varying, three - dimensional spatial fields
of ozone, water vapor, clouds, and aerosols, all
of which have the potential to cause surface and lower to mid-tropospheric temperatures to change relative to one another.
Impact: Replacing old
ozone analyzers at existing stations and adding new sites on the west and east coast
of the U.S. would increase the reliability and scope
of surface
ozone measurements (which may be impacted by industrial activity in Asia).
We downloaded from the NASA Goddard Space Flight Center's website all
of the available monthly averaged
ozone measurements from the NASA Total Ozone Mapping Spectrometer (TOMS) satellite (August 1996 - November 2
ozone measurements from the NASA Total
Ozone Mapping Spectrometer (TOMS) satellite (August 1996 - November 2
Ozone Mapping Spectrometer (TOMS) satellite (August 1996 - November 2005).
The data basis
of observations are total
ozone columns
measurements from three satellite borne instruments: the European satellite sensors GOME (ERS - 2), SCIAMACHY (ENVISAT), and GOME - 2 (METOP - A) are combined and added up to a continuous time series starting in June 1995.
About two years ago Stan Sanders group at JPL tossed a bombshell into our understanding
of stratospheric
ozone depletion, with a new, and much lower
measurement of the chlorine peroxide (ClOOCl) absorption cross-section.