Manchester atmospheric measurements had significant impact on UK response to the 2010 ash crisis
Submitting Institution
University of ManchesterUnit of Assessment
Earth Systems and Environmental SciencesSummary Impact Type
TechnologicalResearch Subject Area(s)
Chemical Sciences: Physical Chemistry (incl. Structural), Other Chemical Sciences
Information and Computing Sciences: Distributed Computing
Summary of the impact
Technology developed at UoM on clouds and aerosols proved vital in
deriving ash mass concentrations during the 2010 eruption of the Iceland
volcano, verifying the Met Office model that was defining the airspace
exclusion zone and predict ash loadings for the Civil Aviation Authority.
The shutdown of airspace cost the airline industry worldwide an estimated
$1.7bn, reaching $400m per day on April 19th. Reassurance
provided by our verification allowed lifting of flight restrictions which
had the immediate effect of re-opening airspace, relieving the impact on
hundreds of thousands of people globally, leading to an estimated global
saving to the industry of $10bn The approach has resulted in new long term
airborne response capability at the Met Office.
Underpinning research
This research took place at The Centre for Atmospheric Sciences,
University of Manchester since 2003. The key researchers were:
Professor Martin Gallagher (1993-) Professor of Atmospheric Physics
Dr Keith Bower (1993-) Senior Research Fellow
Professor Hugh Coe (1997-) Professor of Atmospheric Composition
Dr James Dorsey (2000-) Research Fellow
Dr Paul Connolly (2006-) Senior Lecturer
Professor Geraint Vaughan (2005-) Professor of Atmospheric Science
Over the past decade, research at Manchester's Centre for Atmospheric
Sciences has established world-leading capability in measuring and
interpreting cloud and aerosol properties from ground- based and airborne
platforms. This was augmented by further research [4, 6] during the
Eyafyallajökull eruption to address specific challenges relevant to ash
detection. Key findings/insights were:
- Better calibration techniques for cloud particle imager probes. These
have enabled more accurate measurement of the sizes of cloud particles
and improved our ability to image them correctly. For example, as cloud
particles move through the imaging region their images may become
blurred, leading to mis-sizing. Our work has developed methods for
correcting and improving protocols for using these probes [1].
- Improved analysis and interpretation methods for mixed-phase cloud
data. Our team has developed improved ways of processing cloud
microphysics data through efficient computational data analysis and the
combination of very large, multi-dimensional data sets to more
rigorously probe cloud microphysical phenomena from airborne platforms,
as first evidenced during the EMERALD experiment [2]. These methods have
been rigorously optimised and validated using cloud nucleation
experiments at the EU AIDA large chamber facility e.g. [3].
- Derivation of ash mass from airborne measurements during the
Eyafyallajökull eruption using cloud microphysics probes. During the
volcanic eruption, we deployed our cloud microphysics probes to measure
ash particles. Ash has very different densities and refractive indices
to cloud water or ice and our research during the eruption showed that
the probes were capable of delivering reliable ash mass loading, which
we validated using off-line analysis of filter samples [4].
- Development of Raman LiDAR to measure aerosols and water vapour in the
troposphere, in collaboration with European colleagues, and the
application of Raman lidar measurements together with wind profiling
radars to study atmospheric processes [5].
- A method of deriving ash mass continuously using a combination of
LiDAR and sun photometer. This research, conducted during the eruption,
used the expertise developed by the Manchester LIDAR group, to provide a
retrieval of the ash mass as a function of altitude [6]. Our work also
showed that exploiting the ability of Raman LiDAR to separate
measurements of optical depth and backscatter of the ash was
particularly important in determining detailed measurements of particle
properties.
References to the research
The research outputs have been published in influential international
journals.
Key outputs:
1) Connolly, P. J., Flynn, M. J., Ulanowski, Z., Choularton, T. W.,
Gallagher, M. W., and Bower, K. N.: Calibration of the cloud particle
imager probes using calibration beads and ice crystal analogs: The depth
of fb01eld, J. Atmos. Ocean. Tech., 24, 1860-1879, 2007 [times cited: 26
(ISI)] doi:10.1175/JTECH2096.1
2) Connolly, P. J., O. Möhler, P. R. Field, H. Saathoff, R. Burgess, T.
Choularton, and M. Gallagher, Studies of heterogeneous freezing by three
different desert dust samples Atmos. Chem. Phys., 9, 2805-2824, 2009.
[times cited 45 (ISI)] doi:10.5194/acp-9-2805-2009
3) Johnson, B., et al. (2012), In situ observations of volcanic ash
clouds from the FAAM aircraft during the eruption of Eyjafjallajökull in
2010, J. Geophys. Res., 117, D00U24, doi:10.1029/2011JD016760.
[times cited: 9 (ISI)] Supporting outputs:
4) Gallagher, M. W., Connolly, P. J., Whiteway, J., Figueras-Nieto, D.,
Flynn, M., Choularton T. W., Bower, K. N., Cook, C., Busen, R., and
Hacker, J.: An overview of the microphysical structure of cirrus clouds
observed during EMERALD-1, Quart. J. Roy. Meteorol. Soc., 24, 1143-1169,
2005. [times cited 25 3.33 (ISI)] doi: 10.1256/qj.03.138
5) di Girolamo, P., D. Summa, M. Cacciani, E. G. Norton, G. Peters and Y.
Dufournet. Lidar and radar measurements of the melting layer: observations
of dark and bright band phenomena . Atmos. Chem. Phys., 12, 4143-4157,
2012. [times cited: 0 (ISI)] DOI: 10.5194/acp-12-4143-2012,
6) Devenish B.J., Thomson D.J., Marenco F., Leadbetter S.J., Ricketts H.,
and Dacre H.F., A study of the arrival over the United Kingdom in April
2010 of the Eyjafjallajökull ash cloud using ground-based lidar and
numerical simulations, Atmos. Environ., Vol. 48, 152-164, 2012 [times
cited: 13 (ISI)] doi
10.1016/j.atmosenv.2011.06.033
Details of the impact
"Without a doubt, the strong and close working relationship that exists
between the University of Manchester and the Met Office was a significant
benefit to the Met Office, the CAA, the aviation industry and the general
public as it allowed swift state-of-the-art validation of model forecasts
and satellite retrievals." Dr Jim Haywood, Met Office supporting
letter [A]
Context
On April 14 2010, the eruption of Iceland's Eyafjallajökull volcano
intensified and large quantities of ash began to be ejected into the
atmosphere, reaching UK airspace on the morning of April 15. During this
period, the Met Office's London Volcanic Ash Advisory Centre (VAAC) was
tasked with delivering information on affected regions of the atmosphere
to the Civil Aviation Authority (CAA) using numerical dispersion
modelling. As a result of these model predictions, the International Civil
Aviation Organization (ICAO) guidance, based on a zero threshold for ash
in air, was that it would no longer support service to commercial air
traffic into the affected region. As a result of the impact on the
industry, the VAAC predictions became the subject of intense scrutiny from
the airlines and it became imperative to verify the accuracy of the
forecasts.
Pathways to Impact
The Centre for Atmospheric Sciences has a long track record of developing
ground based and airborne instruments for sensing aerosol and cloud
properties and it has applied these to a wide range of atmospheric
research problems over the last decade and more. This leading research has
meant CAS hosts the aerosol and cloud physics measurement capability for
the NERC National Centre for Atmospheric Science (NCAS) on the FAAM
aircraft in Manchester and was therefore central to the volcanic ash
response during the eruption. The combination of the development of cloud
physics probes and lidars and their application has placed this group as
international leaders in the field and it is this research strength and
experience that enabled the group to rapidly respond to the National Civil
Emergency through the novel application of instrumentation and
interpretation of the data and having the capability to develop the
methods rapidly at the time of the crisis to apply them to a new research
problem.
Prior to the deployment of the FAAM aircraft for the response, the first
British detection of the ash cloud over the UK was from Manchester's LiDAR
system at Cardington on 15 April [B]. The data was immediately relayed to
the Met Office's London Volcanic Ash Advisory Centre. At the Capel Dewi
field facility, the Raman and mobile DIAL lidars were operated by
Manchester for NCAS [F] alongside a Met Office sun photometer to derive
ash mass throughout the eruption. To verify the model predictions during
the first week of the eruption, the NERC Dornier 228 aircraft was
mobilised but initially did not have the measurement capability to detect
ash particles. NERC asked Manchester's Centre for Atmospheric Sciences to
install and operate its cloud physics probes for this purpose [F]. From
April 16 until April 23 the Dornier flew five flights into the ash plume.
These measurements provided initial verification of the Met Office model.
During the first week of the eruption there was no safe operating limit
for ash and therefore the no-fly zone was extensive, severely restricting
air traffic. On April 20 the Civil Aviation (CAA), in cooperation with
engine manufacturers and regulators, was able to agree new procedures
which allowed flights into areas of ash with concentrations predicted by
VAAC to be below 2000 03bcgm-3, with extended maintenance
procedures to be applied for concentrations above 200 03bcgm-3.
The CAA technical report [C] details how the technical basis for the
decision was significantly influenced by the data from Manchester's Centre
for Atmospheric Science (CAS) airborne and LiDAR measurements.
The introduction of this safe operating limit set further challenges for
the Met Office model, which from this point on needed to deliver accurate
and verifiable ash mass forecasts. CAS performed intensive LiDAR
monitoring from the Aberystwyth site throughout the period of the
eruption. These measurements were used by the Met Office, in conjunction
with its sun photometer, to deliver estimates of ash mass. This ultimately
provided the main verification of the Met Office model, although as the
methodology was indirect, direct measurements were still required to
provide evidence that the approach was robust.
The Facility for Airborne Atmospheric Measurements (FAAM) had its
aircraft operational by April 20 and flew five flights up until May 18.
CAS, using the FAAM aircraft, delivered measurements of the size
distribution of the ash particles and used this to develop a method with
the Met Office of assessing ash mass. This data, coupled with shape
analysis delivered by analysis of ash on filters by the Manchester
researchers, was used to confirm the assumptions made using the ground
based and satellite remote sensing retrievals of ash mass and so verify
the Met Office model development. This work increased the model
reliability and the CAA was able to vastly reduce the region of closed
airspace, allowing commercial air traffic around northern Europe to be
effectively re-routed and to return to near full operation.
Reach and Significance
Manchester data saves airline industry billions
The ability of CAS to rapidly respond and provide robust verification,
allowed policy change to be implemented quickly, leading to a reduction in
the number of days affected, the total financial losses and also
disruption to the lives of UK nationals at home and overseas. The shutdown
of airspace was estimated to cost the airline industry worldwide $400m per
day at the height of the closures and caused a total loss of revenue to
the industry of $1.7bn [D]. From April 20 onwards, the new procedures had
the immediate effect of re-opening airspace and it remained substantially
open up to the end of the eruption around 21 May except for a brief and
predicted period between 3 and 5 May. It can be estimated that the
implementation of the new ash thresholds produced a saving of up to $10bn
to the global airline industry, based on extrapolating the average daily
financial losses during the first 6 days before the new thresholds were
introduced throughout the remaining active phase of the eruption. The
University of Manchester measurements played a vital role by providing the
Met Office with verification of their forecast model to allow such a
threshold to be implemented.
Manchester team advises Government
Throughout this time Manchester provided advice directly to the
Government as Professor Coe was a member of the Government Office for
Science's Scientific Advisory Group in Emergencies (SAGE), which reported
through the Chief Scientist to COBRA and the Cabinet Office throughout and
following the event [E]. SAGE advised the Government of the issues and
risks surrounding the on-going volcanic ash event, the necessary
predictive capability at the time and in the future and sought to
establish the risk of future events. Since June 2012, the responsibility
for reviewing volcanic ash threat on behalf of the Government has passed
to the Volcanic Ash Observation Review Group (VAORG), which reports to the
Department for Transport. Professors Vaughan and Coe are members of VAORG.
Professor Vaughan has also advised the Met Office on the specification of
their lidar network and is evaluating the tenders as an external advisor.
Manchester measurement capability taken up by Met Office Volcano
Response Aircraft Facility
An outcome of the SAGE reports was the need for a ground based lidar
network and an airborne volcano response facility that was capable of
delivering a similar response to that provided by the FAAM aircraft on a
continuous, year on year basis. The Met Office has taken on this role and
commissioned lidars and an aircraft for the purpose. The technologies
employed are exactly those supplied by Manchester during the response and
the developed capability is now being maintained operationally should
further eruptions affect airspace over the UK VAAC region [A].
Sources to corroborate the impact
Corroborating information:
A. Letter from Aerosol Research Manager, Met Office, corroborates the
link between Manchester research with cloud physics probes and LIDAR and
their application to the Met Office response during the ash cloud event.
B. A pdf of a web document describing the initial airborne response to
the ash cloud by the NERC aircraft, supported by Manchester Centre for
Atmospheric Sciences, as part of the National Centre for Atmospheric
Sciences contribution to the national response.
http://www.ncas.ac.uk/index.php/en/currentnews/archived-news-2010/86-may-2010-ncas-
response-to-the-eyjafjallajoekull-eruption-2010
C. A pdf of a summary of international teleconferences focused on
revising the agreed safety position of engine manufacturers with respect
to volcanic ash. Chaired by Padhraic Kelleher, Head of Airworthiness, UK
CAA, 5 May 2010
http://www.caa.co.uk/docs/2011/Teleconferences%20log.pdf
D. IATA Economics Risk Analysis of the impact on industry operations and
revenues from the eruption of Iceland's Eyjafjallajokull volcano in April
2010 (downloaded 18th Dec 2012) http://www.iata.org/whatwedo/Documents/economics/Volcanic-Ash-Plume-May2010.pdf
E. A pdf of publically available minutes of the Government Office for
Science Scientific Advisory Group for Emergencies (SAGE), which met 4
times between 21st April and 24th June. http://www.bis.gov.uk/assets/goscience/docs/s/10-1371-sage-volcanic-ash-minutes-21-april-2010,
http://www.bis.gov.uk/assets/goscience/docs/s/10-1372-sage-volcanic-ash-minutes-5-may-2010,
http://www.bis.gov.uk/assets/goscience/docs/s/10-1373-sage-volcanic-ash-minutes-19-may-2010,
http://www.bis.gov.uk/assets/goscience/docs/s/10-1374-sage-volcanic-ash-minutes-24-june-2010
F. Letter from National Centre for Atmospheric Science NCAS Director
verifying that the NCAS and NERC aircraft activity do indeed relate to
Manchester measurements.