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Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component in thunder-storm charging and discharging processes (e.g., Loeb,1965; MacGorman and Rust,1998; Rakov andUman,2003). Many studies have been conducted to investigate the onset condition and the characteristics of corona discharges from water drops and ice particles. 19 Septem ber,2009 60940 60960 60980 61000 61020 61040 61060 61080 21:07:12 21:36:00 22:04:48 22:33:36 23:02:24 23:31:12 0:00:00 UT Pressure 39500 40000 40500 41000 41500 42000 42500 Count rate Aragats pressure ArNM 4 O ctober,2010 61360 61370 61380 61390 61400 61410 61420 61430 61440 16:19:12 16:48:00 17:16:48 17:45:36 18:14:24 18:43:12 19:12:00 UT Pressure 37000 37500 38000 38500 39000 39500 40000 40500 41000 Count rate Aragats P ressure ArNM

Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

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Page 1: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul

Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component in thunder-storm charging and discharging processes (e.g., Loeb,1965; MacGorman and Rust,1998; Rakov andUman,2003). Many studies

have been conducted to investigate the onset condition and the characteristics of corona discharges from water drops and ice particles.

19 September, 2009

60940

60960

60980

61000

61020

61040

61060

61080

21:07:12 21:36:00 22:04:48 22:33:36 23:02:24 23:31:12 0:00:00

UT

Pres

sure

39500

40000

40500

41000

41500

42000

42500

Coun

t rate

Aragats pressure ArNM

4 October, 2010

61360

61370

61380

61390

61400

61410

61420

61430

61440

16:19:12 16:48:00 17:16:48 17:45:36 18:14:24 18:43:12 19:12:00

UT

Pres

sure

37000

37500

38000

38500

39000

39500

40000

40500

41000

Coun

t rate

Aragats Pressure ArNM

Page 2: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

21 May, 2009

61450

61500

61550

61600

61650

61700

61750

15:00 15:28 15:57 16:26 16:55 17:24 17:52 18:21

UT

Pres

sure

38500

39000

39500

40000

40500

41000

41500

Coun

t rate

of ne

utron

s

Aragats pressure (impuls) ArNM

3 June, 2009

61480

61490

61500

61510

61520

61530

61540

61550

61560

61570

14:24 14:52 15:21 15:50 16:19 16:48 17:16 17:45 18:14

UT

Pres

sure

(in im

puls)

-4

-2

0

2

4

6

8

10

Coun

t rate

(%)

Aragats Pressure SAragats Sevan(100)

Page 3: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

7 0ctober, 2012

-3-2-10123456789

101112

13:37 14:06 14:35 15:04 15:33 16:01 16:30

UT

Coun

t rate

(%) a

nd Sp

eed

of W

ind

696.6

696.7

696.8

696.9

697

697.1

697.2

697.3

697.4

Pres

sure

(mb)

Cube middle Aragats speed of wind Aragats pressure

8 October, 2012

-25

-20

-15

-10

-5

0

5

10

15

20

25

30

16:19 16:33 16:48 17:02 17:16 17:31 17:45 18:00 18:14

UT

EF, C

ount

rate(%

) and

Sp

eed

690.5

691

691.5

692

692.5

693

693.5

Pres

sure

Aragats, Electric Field Cube with veto Speed of wind Pressure

Page 4: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

Enhancement and deficit of Muon > 5 GeV during thunderclouds?

4 October, 2010

-40

-30

-20

-10

0

10

20

30

40

18:07 18:14 18:21 18:28 18:36

UT

Ele

ctri

c fi

eld

-25

-20

-15

-10

-5

0

5

10

15

20

25

Co

un

t ra

te o

f m

uo

ns

(%)

Aragats Ef Ar muons>5GeV

4 October, 2010

-40

-30

-20

-10

0

10

20

30

40

50

17:28 17:42 17:57 18:11 18:25 18:40

Co

un

t ra

te (

%)

AMMM(outside)7MeV muons > 5 gev

Page 5: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

3 June, 2009

-2

0

2

4

6

8

10

12

15:50 15:57 16:04 16:12 16:19 16:26 16:33 16:40 16:48

muon>5GeV >10MeV

9 May, 2011

-2.00

-1.00

0.00

1.00

2.00

3.00

4.00

5.00

8:52 9:07 9:21 9:36 9:50 10:04 10:19 10:33

Coun

t rat

e (%

)

Outside detector Muons>5 GeV

Page 6: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

27 May, 2011

-2

0

2

4

6

8

10

12

14

16

18

20

12:00 12:28 12:57 13:26 13:55 14:24

UT

Co

un

t ra

te (

%)

AMMM(outside)>7 MeV AMMM(muons > 5 GeV)

26 August, 2010

-3.00

-2.00

-1.00

0.00

1.00

2.00

3.00

4.00

5.00

9:21 9:50 10:19 10:48 11:16 11:45

UT

Co

un

t ra

te (

%)

AMMM(outside) AMMM(muons>5GeV)

Page 7: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

19 April, 2012

-40

-30

-20

-10

0

10

20

30

40

50

12:43:12 12:50:24 12:57:36 13:04:48 13:12:00 13:19:12 13:26:24 13:33:36

UT

Va

lue

of

Ele

ctr

ic F

ield

-1.5

-1

-0.5

0

0.5

1

1.5

2

Co

un

t ra

te o

f T

GE

pa

rtic

les

Nor Amberd`s Boltek NAMMM(1,0)

Page 8: Ningyu Liu, Joseph R.Dwyer, Hamid K.Rassoul Corona discharges from thundercloud hydrometeors (i.e., water droplets and iceparticles) are an important component

8 January, 2013

-20

-15

-10

-5

0

5

10

15

20

25

30

35

40

1:38 1:40 1:41 1:43 1:44 1:45 1:47 1:48

UT

Ele

ctri

c fi

eld

-10

-8

-6

-4

-2

0

2

4

6

8

10

Co

un

t ra

te (

%)

Aragats EF Ar SEVAN(100) Ar Sevan(middle) Aragats (Geiger) Stand(100)