Abbreviations and glossary

1,25(OH)2D1,25-Dihydroxyvitamin D
25(OH)D25-Hydroxyvitamin D
AKActinic keratosis
AOArctic oscillation. A large-scale variation in Arctic wind patterns
AODAerosol optical depth
APaseAlkaline phosphatase
APCAntigen presenting cell
ASLAbove sea level
BCCBasal cell carcinoma(s)
BrBromine. An ozone-depleting chemical
BrOBromine monoxide
BSWFBiological spectral weighting functions
BWFBiological weighting function
CASChemical Abstracts Service
CATCatalase
CCCortical cataract(s)
CCMChemistry-climate model. Used to predict future changes in atmospheric composition
CDFAChlorodifluoroacetic acid
CDKClimatic droplet keratopathy
CDOCColoured dissolved organic carbon
CDOMColoured (or chromophoric) dissolved organic matter
CFCChlorofluorocarbon. Ozone-depleting substances (e.g. CFCl2 radical, and dichlorodifluoromethane or Freon-12 (CCl2F2)), now controlled under the Montreal Protocol
CHContact hypersensitivity
CH4Methane. A greenhouse gas
CIECommission Internationale de l'Eclairage (International Commission on Illumination)
ClChlorine. An ozone-depleting substance
CMCutaneous melanoma
COCarbon monoxide
CO2Carbon dioxide. A greenhouse gas
COSCarbonyl sulfide
CPDCyclobutane pyrimidine dimer
CuCopper, Cu(I) and Cu(II) being different oxidation states
DICDissolved inorganic carbon
DMSDimethylsulfide
DMSPDimethylsulfoniopropionate
DNADeoxyribonucleic acid
DOCDissolved organic carbon
DOMDissolved organic matter
DONDissolved organic nitrogen
DSBDouble strand break
DTHDelayed type hypersensitivity
DUDobson unit. Used for the measurement of total column ozone (1 DU = 2.69 × 1016 molecule cm−2)
EAEExperimental allergic encephalitis
EDUCEEuropean Database for Ultraviolet Radiation Climatology and Evaluation
EESCEquivalent Effective Stratospheric Chlorine. A term used to represent the total chlorine concentration in the stratosphere from all sources of ozone-depleting substances (including CFCs, HCl, Cl2, ClONO2, etc.) and a scaled contribution from other halocarbons and bromine, taking its ODP into account
ENSOEl Niño Southern Oscillation. A large-scale climate variability in the Pacific region
EPEarth Probe. A NASA satellite
EPAEnvironmental Protection Agency (USA)
EVEpidermodysplasia verruciformis
FeIron, Fe(II) and Fe(III) being different oxidation states
FMIFinnish Meteorological Institute
GHGGreenhouse gas
Glu IA pathogenesis-related (PR) protein
GSTGlutathione-S-transferase
GWPGlobal warming potential. A measure of the warming effectiveness of a gas compared with CO2
HALSHindered Amine Light Stabilizer
HCFCHydrochlorofluorocarbon. Interim replacements for CFCs with small ozone depletion potential (e.g. R22: chlorodifluoromethane, CHClF2), to be phased out
HFCHydrofluorocarbon. Long-term replacements for CFCs
HFOHydrofluoro-olefin
HgMercury, Hg(0)aq and Hg(II) being different oxidation states
HIVHuman immunodeficiency virus
HPVHuman papillomavirus
HSVHerpes simplex virus
HY5Transcription factor HY5, which is a key downstream effector of the UVR8 (UV-regulatory protein) pathway
IBDInflammatory bowel disease
ILInterleukin
Ink4aMurine inhibitor of kinase 4a protein (gene when in italics)
IPCCIntergovernmental Panel on Climate Change
IPFImmune protection factor
kDaKilodalton
KNMIDutch National Institute for Weather, Climate and Seismology (Netherlands)
Lipid radical
MAAsMycosporine-like amino acids
MbMegabase, equal to 1 million base pairs
MC1RMelanocortin 1 receptor
MHCMajor histocompatibility complex
MSMultiple sclerosis
N2ONitrous oxide. A greenhouse gas that is also a source of NO2
NAONorth Atlantic Oscillation. A large-scale variation and redistribution of atmospheric mass in the Atlantic region producing large changes in the Northern hemisphere dynamics
NASANational Aeronautic and Space Administration (USA).
NaTFASodium trifluoroacetate
NCNuclear cataract(s)
NCARNational Centre for Atmospheric Research (USA)
NHNorthern Hemisphere
NIMBUS-7A NASA satellite
NIVRNetherlands Agency for Aerospace Programmes
NMHCsNon-methane hydrocarbons
NMSCNon-melanoma skin cancer
NONitric oxide. An ozone-depleting gas
NO2Nitrogen dioxide. An ozone-depleting gas
NOAANational Oceanic and Atmospheric Administration (USA)
NOECNo observed effect concentration
NOxNitrogen oxides
O3Ozone
OCSCarbonyl sulfide
ODPOzone depletion potential. The ratio of the impact on ozone of a chemical compared to the impact of a similar mass of CFC-11. Thus, the ODP of CFC-11 is defined to be 1.0
ODSOzone-depleting substance(s) (e.g. CFCs)
˙OHHydroxyl radical. An important atmospheric cleaning agent
OMIOzone Monitoring Instrument. On board the Aura satellite
OTROrgan transplant recipient
PPhosphorous
PAHPolycyclic Aromatic Hydrocarbon(s)
PAMPulse amplitude modulated (fluorescence)
PARPhotosynthetically Active Radiation, 400–700 nm waveband
PAUR IIPhotochemical Activity and solar Ultraviolet Radiation campaign 2
pCO2Partial pressure of carbon dioxide
PECPredicted environmental concentration
PERPhotoenzymatic repair
PgPetagram (1 × 1012 grams)
PHR1 The gene encoding CPD photolyase
PNECPredicted no effect concentration
POCParticulate organic carbon
POMParticulate organic matter
PRPathogenesis-related proteins
PSCPosterior subcapsular cataract(s)
PSCPolar stratospheric cloud. Ice crystals which form at high altitudes in Polar regions when the temperature is below a critical threshold
PSIPhotosystem I
PSIIPhotosystem II
PtcMurine patch protein (gene when in italics)
PTCHHuman patch protein (gene when in italics)
QBOQuasi-biennial oscillation. A shift in wind patterns – especially over the tropics – with a period of approximately 2.2 years
RARheumatoid arthritis
Radiative forcingA measure of the influence a factor (e.g. GHGs, ice albedo, tropospheric aerosols, etc.) has in altering the balance of incoming solar and outgoing infrared irradiance (W m−2) in the Earth-atmosphere system. It is an index of the importance of the factor as a potential climate change mechanism. Radiative forcing is approximately proportional to temperature changes at Earth's surface, so a positive radiative forcing is associated with heating in the troposphere
RAFRadiation amplification factor. A measure of sensitivity to ozone change
ROSReactive oxygen species (˙OH for example)
RTRadiative transfer
SAGEStratospheric Aerosol and Gas Experiment. A satellite-based instrument
SCCSquamous cell carcinoma
SHSouthern hemisphere
SODSuperoxide dismutase
SZASolar zenith angle. The angle of the sun away from the vertical; at noon, it represents the highest point that the sun reaches
TFATrifluoroacetic acid
Th1T-helper 1
Th2T-helper 2
TOMSTotal Ozone Mapping Spectrometer. A satellite-based instrument
Treg cellT-regulatory cell
TroposphereLowest part of the earth's atmosphere (0–16 km)
UCAUrocanic acid
UNEPUnited Nations Environment Programme
UVUltraviolet. Wavelengths from 100 nm to 400 nm. Ozone and other atmospheric gases progressively absorb more and more of the radiation at wavelengths less than 320 nm. Only those greater than 290 nm are transmitted to the Earth's surface
UV-AElectromagnetic radiation of wavelengths in the 315 to 400 nm range. Weakly absorbed by ozone
UV-BElectromagnetic radiation of wavelengths in the 280 to 315 nm range. Strongly absorbed by ozone
UV-CElectromagnetic radiation of wavelengths in the 100 to 280 nm range. Solar UV-C is not transmitted to Earth's surface
UVEryErythemally-weighted UV irradiance, where the irradiance is weighted by the erythemal action spectrum
UVIUV index. A measure of erythemally-weighted UV for providing information to the public. UVI values greater than 10 are considered “extreme” by the WHO. If UV-Ery is specified in units of W m−2, then UVI = 40 × UV-Ery
UVR8UV-regulatory protein
VDRVitamin D receptor
VOCVolatile organic compound(s)
WMOWorld Meteorological Organization
WOUDCWorld Ozone and UV Data Centre
XPXeroderma pigmentosum

This journal is © The Royal Society of Chemistry and Owner Societies 2011
Click here to see how this site uses Cookies. View our privacy policy here.