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Manish Naja Aryabhatta Research Institute of Observational Sciences [ARIES], Nainital International workshop on Changing Chemistry in Changing Climate: Monsoon, IITM, Pune [1-3 May, 2013]

Manish Naja - C4

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Page 1: Manish Naja - C4

Manish NajaAryabhatta Research Institute of Observational Sciences

[ARIES], Nainital

International workshop on Changing Chemistry in Changing Climate: Monsoon,

IITM, Pune [1-3 May, 2013]

Page 2: Manish Naja - C4

The IGP region is undoubtedly one of the most polluted region in

India.

Most densely populated region

Home to large agricultural activity, hence crop residue burning

This region is also dominated by western disturbances.

The Central Himalayas is in the transition region from tropical to

mid-latitude tropopause and characterized by the tropopause-break.

Ghude et al., JGR 2013

Page 3: Manish Naja - C4
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Population Density

Devasthal – 29.4N, 79.7E, ~ 2450 m

Nainital – 29.4N, 79.5E, ~ 1958 m

Pantnagar – 29.0N , 79.5E, ~ 231 m

Dehradun – 30.3N, 78E, ~640 m

IGP – 1000-more persons/km2

Nainital – 25-100 persons/km2

Page 5: Manish Naja - C4

Aerosols

Trace Gases

Lidar

Met Tower

ST Radar (upcoming)

Observational facilities at ARIES

– AOD (MWR and Microtops)

– Black Carbon

– Aerosols number concentrations

– Particulate Matter

– Pollutants (Ozone, CO, NO, NOy, CH4 , NMHCs, SO2)

– Balloon-borne observations of ozone and met parameters

– Greenhouse gases (CO2, CH4, N2O and SF6)

– Aerosols

Page 6: Manish Naja - C4

Northern India is under the

influence of air-masses arriving

from Africa/Europe and Marine

regions and also affected by

emissions from IGP.

Nainital: A Regional

Representative site

for N. India / Central Himalaya

Kumar, Naja et al., JGR 2010

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Pantnagar(IGP site)

Nainital (Central Himalayan site)

Both the sites are about 30 km apart

Page 10: Manish Naja - C4

Nitrogen Oxide (NOx )

Carbon Monoxide (CO)

IGP site (Pantnagar)

Page 11: Manish Naja - C4

Note the

differences

between

Pantnagar and

Nainital

Daytime and Nighttime

correlation between ozone at

Pantnagar and Nainital

Ojha, Naja et al., JGR 2012

Page 12: Manish Naja - C4

Comparison with OMI, TES and Model

Model captures observed ozone

seasonality but overestimates ozone

levels

Ojha, Naja et al., JGR 2012

Page 13: Manish Naja - C4

Accumulated Ozone Exposure Index (AOT40)

at two IGP sites

AOT40 values are significantly higher than criticallevel (3000 ppbv*hr) Threat for vegetationsover this region.

Page 14: Manish Naja - C4

CH2O/ NOy<0.28 VOC limited regime

>0.28 NOx limited regime

Mostly NOx limited region

Kumar, Naja et al., GMD 2012

Ozone control

WRF-Chem Simulation

But IGP show

tendency of VOC

limited region,

mainly in

Winter/Spring !!

Page 15: Manish Naja - C4

Black Carbon (ng/m3)

0 1000 2000 3000 4000 5000 6000 7000

CO

(p

pb

v)

0

100

200

300

400

500

600

CO = (0.07 * BC) + 115

r2 = 0.95

March 2007

Black Carbon (ng/m3)

0 1000 2000 3000 4000 5000 6000

Ozo

ne

(pp

bv)

30

40

50

60

70

80

90

O3 = (0.006 * BC) + 41

r ² = 0.79

CO & BC

O3 & BCInfluence of fresh combustion

Automobile combustion

Such influences/correlations are

seen away from the source regions

Biomass burning event

Page 16: Manish Naja - C4

Mt Abu

Nainital(Biomass burning, photochemistry)

Kumar, Naja et al., JGR 2010

Ojha, Naja et al., JGR 2012

Page 17: Manish Naja - C4

[2004-05]

Time (IST)

0 2 4 6 8 10 12 14 16 18 20 22 24

Av

erag

e O

zon

e (p

pb

v)

20

40

60

80

Ozone at Boudha, Nepal

Ozone at Nainital

Pandey et al., 2009

Page 18: Manish Naja - C4

Oct 04

Jan 05

CO at Boudha, Nepal

Pandey et al., 2009

Time (IST)

0 2 4 6 8 10 12 14 16 18 20 22 24

CO

(p

pb

v)

100

200

300

400

500

600

700

Nainital

Page 19: Manish Naja - C4

Pantnagar

Nainital

Jan-Feb

0 4 8 12 16 20 24

Ozo

ne

(pp

bv

)

0

20

40

60

80

Kathmandu

Nainital

Jan-Feb

Hours

0 4 8 12 16 20 24

CO

(p

pb

v)

0

500

1000

1500

2000

Nainital

Kathmandu

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Radiosonde

AMF1 set up during GVAX (Ganges Valley

Aerosols Experiment) at ARIES Nainital

Page 23: Manish Naja - C4

GVAX Balloon flights (ARM Mobile Facility-1, DOE, USA)

Flight Time Jan Feb Mar Jun Jul Aug Sep Oct Nov Dec

IST 0530 hrs 30 26 30 3 31 29 28 25 26 29 257

IST 1130 hrs 30 27 30 6 29 30 30 30 30 30 272

IST 1730 hrs 31 29 28 3 30 27 30 31 29 31 269

IST 2330 hrs 31 30 28 0 28 26 30 31 29 30 263

122 112 116 12 118 112 118 117 114 120 1061

Table-1 Successful GVAX balloon flights during June 1st 2011 – March 31st 2012

The high frequency radiosonde (1061)

measurements were carried out during Ganges

Valley Aerosol eXperiment 2011-2012.

Page 24: Manish Naja - C4

Wind Speeds

Wind speeds are highest in winter (~ 80m/s)

months, indicating a presence of subtropical jet.

Page 25: Manish Naja - C4

NIES, Tsukuba, Japan

N2O

SF6

CH4

CO2

CO

Page 26: Manish Naja - C4

WMO GAW Bulletin no 8, Nov 2012

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……… it is in the tropics

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Highlights: Studies on winds, monsoon dynamics and Troposphere Stratosphere exchange Frequency : 206.5 MHz Area Covered : 30x30 m Continuous and high resolution winds

~10 min for full profile 50 to 300 m Velocity resolution : 0.1 m/s to 2 m/s

Page 29: Manish Naja - C4

RAWEX-GVAX

Regional Aerosols Warming Experiment

Ganges Valley Aerosols ExperimentA multi institutional project

DOE (USA), ISRO, IISc and ARIES

A major international initiative after about 13 years

Page 30: Manish Naja - C4

15 Dec - 25 Dec 2010

12/16/201012/18/2010

12/20/201012/22/2010

12/24/201012/26/2010O

zon

e (p

pbv

)/R

elat

ive

Hum

idit

y (

%)

0

20

40

60

80

100

120

140

160NTL PNT

Relative Humidity