Projects per year
Abstract
High frequency, in situ observations from 11
globally distributed sites for the period 1994–2014 and archived air
measurements dating from 1978 onward have been used to determine the
global growth rate of 1,1-difluoroethane (HFC-152a, CH3CHF2).
These observations have been combined with a range of atmospheric
transport models to derive global emission estimates in a top-down
approach. HFC-152a is a greenhouse gas with a short atmospheric lifetime
of about 1.5 years. Since it does not contain chlorine or bromine,
HFC-152a makes no direct contribution to the destruction of
stratospheric ozone and is therefore used as a substitute for the ozone
depleting chlorofluorocarbons (CFCs) and hydrochlorofluorocarbons
(HCFCs). The concentration of HFC-152a has grown substantially since the
first direct measurements in 1994, reaching a maximum annual global
growth rate of 0.84 ± 0.05 ppt yr−1 in 2006, implying a
substantial increase in emissions up to 2006. However, since 2007, the
annual rate of growth has slowed to 0.38 ± 0.04 ppt yr−1 in 2010 with a further decline to an annual average rate of growth in 2013–2014 of −0.06 ± 0.05 ppt yr−1.
The annual average Northern Hemisphere (NH) mole fraction in 1994 was
1.2 ppt rising to an annual average mole fraction of 10.1 ppt in 2014.
Average annual mole fractions in the Southern Hemisphere (SH) in 1998
and 2014 were 0.84 and 4.5 ppt, respectively. We estimate global
emissions of HFC-152a have risen from 7.3 ± 5.6 Gg yr−1 in 1994 to a maximum of 54.4 ± 17.1 Gg yr−1 in 2011, declining to 52.5 ± 20.1 Gg yr−1 in 2014 or 7.2 ± 2.8 Tg-CO2 eq yr−1.
Analysis of mole fraction enhancements above regional background
atmospheric levels suggests substantial emissions from North America,
Asia, and Europe. Global HFC emissions (so called “bottom up” emissions)
reported by the United Nations Framework Convention on Climate Change
(UNFCCC) are based on cumulative national emission data reported to the
UNFCCC, which in turn are based on national consumption data. There
appears to be a significant underestimate ( > 20 Gg) of “bottom-up”
reported emissions of HFC-152a, possibly arising from largely
underestimated USA emissions and undeclared Asian emissions.
| Original language | English |
|---|---|
| Pages (from-to) | 365-382 |
| Number of pages | 18 |
| Journal | Atmospheric Chemistry and Physics |
| Volume | 16 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 18 Jan 2016 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
-
SDG 13 Climate Action
Research Groups and Themes
- Organic & Biological
- Physical & Theoretical
Fingerprint
Dive into the research topics of 'Global and regional emissions estimates of 1,1-difluoroethane (HFC-152a, CH3CHF2) from in situ and air archive observation'. Together they form a unique fingerprint.Projects
- 3 Finished
-
Verifying national HFC emissions
Rigby, M. L. (Principal Investigator)
4/08/15 → 31/08/22
Project: Research
-
Advanced computing architecture to support the estimation and reporting of UK GHG emissions
Rigby, M. L. (Principal Investigator)
13/11/13 → 13/10/15
Project: Research
-
Towards treaty verification of all non-CO2 greenhouse gasses - Dr Matthew Rigby
Rigby, M. L. (Principal Investigator)
1/01/12 → 31/12/16
Project: Research
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