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RESEARCH INTEREST:

1. Urban Air Pollution and Air Quality Impact Assessment

2. Air Quality Modelling (CALINE4, AERMOD, SMOKE/CMAQ)

3. Tropospheric Chemistry  in the tropic (i.e Ozone)

4. Tropical biogenic emissions 

5. Climate Change and Air Quality

 

 

CURRENT RESEARCH:

 

1. LRGS (LONG TERM RESEARCH GRANT SCHEME)

 

Global Warming : Drivers, Sciences, Impacts and Responses for Sustainability

 

Sub-Project No.3:  Climate Impacts, Vulnerability and Risks: Towards Development of Adaptation Policy

 

This project focusses on three issues:

  1. * Air quality
  2. * Hydrology/Flooding
  3. * Landslide

 

 

 2. SHIVA - Stratospheric ozone: Halogen Impacts in a Varying Atmosphere

This project is an international research project supported by the 7th Framework Programme of the Eurpean Union.  In conjunction with Mala SHIVA Logo This project is an international research project supported by the 7th Framework Programme of the Eurpean Union.  In conjunction with Mala ysian research partners long term measurements will take place across the tropics. In late 2011 a core field campaign will take place in the South China Sea, and along the coastline of Peninsula Malaysia and Borneo using the Sonne Research Vessel, the DLR Falcon aircraft, satellites, and land-based investigation teams.

                                              map

 

SHIVA focuses on four major objectives:

  • 1.  Investigation of the oceanic emission strengths of a suite of halogenated source gases: Here emphasis is put on the production, emission and transport of ODS. Inter-dependencies derived from our own field observations as well as surveys of ongoing work in this area will help establish potential climate sensitivities of VSLS emissions.
  •  
  • 2. Investigation of the atmospheric transport and chemical transformation of halogenated VSLS and their PGs during their journey from the surface to the TTL and finally into the stratosphere. Her a combination of aircraft and balloon observations together with process-oriented meso-scale modeling is used. These investigations are corroborated by space-based remote sensing of marine phytoplankton biomass as a possible proxy for the ocean-atmosphere flux of VSLS.
  •  
  • 3. Investigation of the past, present and likely future trend of the total halogen burden in the stratosphere, which is established from the systematic VSLS emission inventory established under theme 1 and 2. Here the impact of climate-sensitive feedbacks between transport and the delivery of ODS to the stratosphere, and their lifetime within it, is studied using tracer observations and modeling. When all this knowledge is combined, the assessed climate sensitivities will eventually support the construction of future-climate scenarios of VSLS emissions and possible pathways for their delivery to the stratosphere.
  •  
  • 4. Investigation on the impact of long and short-lived halogenated SGs and their inorganic PGs on past, present and future ozone is assessed for the upper troposphere, TTL and global stratosphere. Here global modeling includes the contribution of all ODS, including VSLS (which have hitherto normally been excluded from such models) to past, present and future ozone loss. The sensitivity of natural ODS emissions to climate change parameters investigated under theme 3 is used in combination with standard IPCC climate model scenarios in order to drive measurement-calibrated chemical transport model (CTM) simulations for present and future stratospheric ozone and to better predict the rate, timing and climate-sensitivity of ozone-layer recovery.

 

 

 

Parameters to be measured on the  Falcon aircraft

Chemical species
Comment
Ozone Stratospheric tracer, photochemical product gas, greenhouse gas
Halocarbons (inc VSLS) (1) In situ GC-MS
(2) Whole air samples – analysis on the ground at airport
NO 2, BrO, IO, HONO, CH 2O, C 2H 2O 2 Halogen radicals (VSLS atmospheric degradation products)
Br 2, HBr, ClNO 2 VSLS degradation products
N 2O (nitrous oxide) Greenhouse gas, stratospheric tracer
SF 6 (sulphur hexafluoride) Greenhouse gas, anthropogenic tracer used for dating of stratospheric air
CO (carbon monoxide) Tracer for combustion (pollution, biomass burning)
CO 2 (carbon dioxide) Tracer
H 2O (water vapour) Tracer
NO, NOy Tracer for convective outflow, tracer for anthropogenic pollution, lightning product gas
Peroxyacetyl nitrate (PAN) Tracer for anthropogenic organic pollution, tracer for biomass burning
Perfluorocarbone (e.g. C7F14) Artificial air mass tracer for ship / aircraft - Lagrangian experiment

There will also be measurements of temperature, pressure, wind speed, wind direction, humidity, and altitude. Also, a forward-looking cockpit video camera will record clouds and pollution layers.

Parameters to be measured on the  RV Sonne

Measured Parameter
Comment
In seawater
Halocarbons (inc VSLS) In situ GC-MS
Phytoplankton Size, cell number, species composition
Chlorophyll Concentration and photosynthetic efficiency
Pigments Chic3, peridin, fuco, 19-hex, neox, etc
PCO 2 (dissolved carbon dioxide) Sensorr
PO 2 (dissolved oxygen) Sensor and Winkler titration
Nutrients Nitrate and phosphate
Gas tension Pressure of all dissolved gases in seawater
Salinity Conductivity, Temperature, Depth (CTD) Sensor
Sea surface temperature Conductivity, Temperature, Depth (CTD) Sensor
DMS, N 2O,CH 4 In situ GC and post cruise analysis
Radiation Upward and downward fluxes
In air
Halocarbons (inc VSLS) (1) In situ GC-MS
(2) Whole air samples – analysis on the ground at airport
BrO, IO Halogen radicals (VSLS atmospheric degradation products)
Br and I in aerosol Filter sampling
Ozone, methane, CO 2, H 2O Greenhouse gases; continuous surface measurements (UV absorption instrument and PICARRO cavity ring down spectrometer)
CO (carbon monoxide) Tracer for combustion (pollution, biomass burning)
CH 4 (methane) Greenhouse gas
N 2O (nitrous oxide) Greenhouse gas
OH radicals Determine atmospheric lifetime of VSLS and other trace gases
Non methane hydrocarbons Primary pollutants (anthropogenic tracers)
HCl, ClNO 3, SO 2, HNO 3 Chemical ionisation mass spectrometer, oxidation products
Radiosonde Balloon-borne sondes (up to 30 km altitude)
Vertical temperature, pressure, humidity, wind profiles
Ozonesonde Balloon-borne sondes (up to 30 km altitude)
Vertical profiles of ozone
Water vapour sondes Balloon-borne sondes (up to 30 km altitude)
COBALD sondes (clouds) Balloon-borne sondes (up to 30 km altitude)
Tracer release unit Release of perfluoro-carbons for ship / aircraft 
Lagrangian experiment
Precipitation; In-situ measurements
Standard Ship parameters Position, temperature, pressure, humidity, wind speed and direction, water depth

Halocarbons to be measured during SHIVA (aircraft and ship)

Compund
Lifetime
(Days)
Atmospheric Source / possible climate feedback
Medium and short-lived halocarbons (mixed sources)
CH 3Br
250
Mixed sources including oceanic, biomass burning (BB), vegetation, soils, and anthropogenic. Sensitive to changing land use and climate
CH 3Cl
360
Mixed natural sources including BB and vegetation. Sensitive to changing land use and climate
CH 2Br 2
120
Oceanic, climate sensitive
CHBr 3
26
Oceanic (small anthropogenic source), climate sensitive
CH 2BrCl
150
Oceanic, climate sensitive
CHBrCl 2
78
Oceanic, climate sensitive
CHBr 2Cl
69
Oceanic, climate sensitive
C 2H 5Br
34
Oceanic and anthropogenic, climate sensitive
CH 3I
7
Oceanic and terrestrial, climate sensitive
CH 2ClI
<1 day
Oceanic, climate sensitive
CH 2BrI
<1 day
Oceanic, climate sensitive
CH 2I 2
<1 day
Oceanic, climate sensitive
CH 2Cl 2
14
Mixed sources: anthropogenic and BB, ocean
CHCl 3
150
Mixed sources: anthropogenic, BB, soils, sensitive to changing land use / climate
C 2HCl 3
46
Mainly anthropogenic
C 2Cl 4
99
Mainly anthropogenic (possible oceanic source)
CH 2ClCH 2Cl
70
Mainly anthropogenic
C 2H 5Cl
30
Mainly anthropogenic
Long-lived anthropogenic halocarbons
CFCs
(11, 12, 113, 114, 115)
>45 yrs
Changing stratospheric transport changes fractional halogen release
HCFCs
(22, 142b, 141b)
>9 yrs
Changing stratospheric transport changes fractional halogen release
CH 3CCl 3
5 yrs
Changing stratospheric transport changes fractional halogen release
CCl 4
26 yrs
Changing stratospheric transport changes fractional halogen release
Halons
(1301, 1211, 2402)
>16 yrs
Changing stratospheric transport changes fractional halogen release

 

 

 

 

updated on 2011-07-08 20:04:14 by Justin Sentian, Dr




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