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Human Influence and Climate Change
GHGs and aerosols
internal climate variability
year to year variation in climate caused by internal climate processes
human influence detectable when climate change signal is greater than climate variability
Climate Variability: El Nino Southern Oscillation
main cause of year to year variability in global atmospheric weather patterns affecting climate over many regions
also slightly global mean temperatures
El Nino and La Nina phases
impacts on tropical and global climate
El Nino can cause flooding in tropical South America and dry conditions in South East Asia/Oceania
changes to the atmospheric circulation affect neighbouring regions hence ENSO impacts extend outside of tropics
El Nino
the tropical eastern Pacific becomes unusually warm in winter/spring and this continues for about a year
warm surface water propagates eastward
surface pressure rises in the West and falls in the East
the pressure gradient between East and West Pacific weakens hence the trade winds weaken
Southern Oscillation
region of heaviest rainfall moves eastward
drought in South East Asia, flooding in South America
La Nina
colder than average SSTs in the tropical eastern Pacific
higher than normal pressure in East Pacific, strong PGF, stronger trade winds
low pressure and heavier than normal rainfall in South East Asia
sinking air and drier weather over South America
enhancement of normal conditions
Climate Variability: North Atlantic Oscillation
atmosphere perturbation
Positive Phase of Wintertime NAO
southerly flow from tropics leads to warmer weather in Europe
Negative Phase of Wintertime NAO
cold air from Canada leads to colder weather in Europe
varies year by year
NAO Positive Phase
enhanced southerly flow from tropics keeps cold air in Canada
jetstream and storm track in North Atlantic
strong low pressure in high North Atlantic
warmer and wetter in Northern Europe
drier in Southern Europe and Northern Africa
strong subtropical high pressure
NAO Negative Phase
strong flow of cold air from Canada
jetstream and storm track in mid-Atlantic
weak low pressure in high North Atlantic
colder and drier in Northern Europe
wetter in Southern Europe and Northern Africa
weak subtropical high pressure
Air Pollutants
particulate matter (PM)
usually PM2.5 referred to
PM with aerodynamic diameter <2.5µm
solid or liquid
PM2.5 refers to size, composition varies
either emitted as primary PM, or formed in atmosphere from gases as secondary PM
Ozone (O3)
Nitrogen Dioxide (NO2)
PM2.5 and NO2 often co-emitted (traffic), as well as with CO2
O3 and NO2 in urban environments usually inversely related
Types of Particulate Matter 2.5 (3, 4)
inorganic (nitrate, sulphate, ammonium)
organic (black carbon, organic carbon, dust, sea-salt)
multiple anthropogenic and natural sources
Ozone
major oxidant species in atmosphere
secondary pollutant formed in the atmosphere in the presence of sunlight and precursor emissions
greenhouse gas
Nitrogen Dioxide
also a gaseous oxidant
forms from nitrogen oxide (mainly anthropogenic sources)
The Case for Clean Air
Ella Adoo-Kissi-Debrah
died in 2013, in 2020 Coroner’s court found air pollution ‘made a material contribution’ to her death
first time ever that air pollution was listed as cause of death
air pollution linked to asthma
Ella exposed to excessive amount of NO2 from road traffic (south circular London)
Health Effects of Air Pollution
short term
exacerbation of asthma
cough, wheezing and shortness of breath
long term
stroke
lung cancer
respiratory conditions
cardiovascular disease
reduced life expectancy
estimated that 28-36,000 deaths in UK per year linked to long-term exposure
Anthropogenic Sources of Air Pollution in UK
energy industries
manufacturing industries
construction
residential combustion
road transport
agriculture
etc.
Natural Sources of Air Pollution
smoke particles and gases from volcanoes and wildfires produce PM2.5, PM10, NO2 and O3
methane emissions from wetlands, ruminants, decomposition of organic matter produce O3
Biogenic Volatile Organic Compounds (BVOCs) from certain tree species produce PM2.5 and O3
Air Pollution London 2019
some areas of central London exceed UK annual objective for NO2
large areas of central London exceed WHO guideline for PM2.5
WHO 2021 Guidelines
challenging, especially for PM
5µgm^3 per year
nowhere in London is below this annual limit for PM2.5
Anticyclones and Air Pollution
increase air pollution
high pressure leads to light winds and little atmospheric mixing
reduced vertical dispersion
mostly descending air from above
temperature inversion at the top of the boundary layer limits vertical mixing
no precipitation to aid ‘wet’ removal of PM
strong sunshine allowing photochemical reactions, e.g. to form ozone
Future SSP Scenarios (6)
global emissions of CO2 and of air pollutant emissions and precursors
near term climate forcers (NTCF)
most scenarios show a reduction in global emissions, although there is large diversity between scenarios and regional variation
future methane shows large variation between scenarios, important for ozone formation
large PM2.5 emission reductions in Asia with large emission reduction scenarios
O3 reductions driven by large reductions in precursors (NOx and VOCs)
SSP3-7.0 decrease in PM2.5 in Europe and East Asia, increase in South Asia, Middle East, Nigeria and Uganda regions, increase in O3 across Asia, Africa, South America
Climate Change and Air
climate change and air quality not necessarily hand in hand
reduced sulphur emissions good for air quality, bad for climate change
planting high BVOC trees good for sequestering carbon, bad for air quality
biomass and hydrogen both increase NOx and PM2.5