Mobile system for atmospheric temperature profile monitoring: mobile MTP-5 Mikhail Khaikine1), Arkady Koldaev1), Evgene Kadygrov1), Evgene Miller1) Vladimir Sokolov2) Nikolay Sokolov3) 1) Central Aerological.

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Transcript Mobile system for atmospheric temperature profile monitoring: mobile MTP-5 Mikhail Khaikine1), Arkady Koldaev1), Evgene Kadygrov1), Evgene Miller1) Vladimir Sokolov2) Nikolay Sokolov3) 1) Central Aerological.

Mobile system for atmospheric temperature profile
monitoring: mobile MTP-5
Mikhail Khaikine1), Arkady Koldaev1), Evgene Kadygrov1), Evgene Miller1)
Vladimir Sokolov2) Nikolay Sokolov3)
1) Central Aerological Observatory, Federal Service for Hydrometeorology
and the Environmental Monitoring (Roshydromet) , Moscow, Russia,
e-mail: [email protected]
2) Upper Volga Interregional Territorial Department, Roshydromet, Nijny
Novgorod, Russia
3) The Committee for Environmental Protection and Natural Resources
Management of the Nizhny Novgorod Region, Nijny Novgorod, Russia
Nijny Novgorod
Mobile system for atmospheric temperature profile monitoring: mobile MTP-5
Introduction
Studies of ground temperature
heterogeneity show that the heat island inside
of the city can have heterogeneous structure
so-called "multicupolas". But this assumes, in
turn, the three-dimensional heterogeneity of
temperature profile. Thus, in the city can be
observed different conditions for forming and
destroying the inversions and, therefore, can
be formed different prerequisites for pollution
concentration increase in the Atmospheric
Boundary Layer (ABL).
MMTP-5
Mobile system for atmospheric temperature profile monitoring: mobile MTP-5
The technique and equipment used in the
measurements.
The investigations of space heterogeneity of
atmospheric temperature stratification were
carried out by mobile system MMTP-5 in the
large city Nijny Novgorod and in its suburb in
August-October 2004. The measurements of
temperature profiles were conducted
simultaneously by MMTP-5 and by stationary
MTP-5 installed on the roof of hotel “Oka” at
the altitude 235 m. The special equipment
installed on the mobile system MMTP-5
allowed measuring air pollution concentration.
The results of temperature profile
measurements in 12 points of Nijny Novgorod
and its suburb (5 points) are presented in this
report.
Stationary MTP-5
Mobile system MMTP-5
Mobile system for atmospheric temperature profile monitoring: mobile MTP-5
Main objectives for MMTP-5
1)
Possibility of measurements in different locations with the use
of unique, high cost device
2)
Possibility of making measurements in the immediate vicinity
of sores of air pollution
3)
Possibility of scientific study of features in Urban climate and
correspondent distribution of air pollutions (WMO GURME
project)
4)
Possibility of emergency service with “on site” air pollution
diagnostic and forecast in case of industrial and public
catastrophe
5)
Commercial usage of the system as a rent or lease for
environment protection services in industry and for scientific
groups
MMTP
Mobile system for atmospheric temperature profile monitoring: mobile MTP-5
Features of MMTP-5 construction
1)
Absence of any microwave units inside the car – installation on
the roof of car.
2)
Harsh weather and road condition protection – installation inside
the standard car roof box.
3)
Vibrating protection against car structure vibration and vibration
caused by the road – three levels of vibrating protection:
a) Solid state assembling of microwave radiometer;
b) Vibrating isolation of microwave radiometer and housing
c) Vibrating isolation of the complete system and car body in
transport position
4)
Power supply on the base of standard car battery – set of power
converters and stabilizers
5)
On line time and space location – GPS and GSM modem
integrated in to the process of measurements
MMTP
Pictures in transport position
MMTP
Pictures on operation position
MMTP
Relative positions of
measuring points
Volga
Oka
Measuring points altitude [m]
H[м]
235
250
184
200
155
160
130
150
100
100 100
90
100
92
92
80
86
80
75
85
86
50
12,13
1,2,3
4
0
N1
N2
N3
N4
N5
N6
N7
N8
N9
N10 N11 N12 N13
N0
N 14 N 15 N 16
90
60
Sunrise 07:22
August 6, 2004
1000
30
900
0
Temperature scale
800
-30
O
10 C
-60
Altitude [m]
700
-90
600
-120
500
-150
-180
400
-210
300
-240
200
-270
100
Sun angle [grad]
1100
N1
0
0:00
N2
N3
N4
N5
N9
N7
N11
N10
-300
N12
N8
1:00
Temperature
profile
measured
by MMTP-5
2:00
3:00
4:00
5:00
6:00
7:00
8:00
9:00
N13
-330
-360
Time
10:00[hh:mm]
12,13
1,2,3
4
800
August 7, 2004
Temperature scale
10OC
700
600
Altitude [m]
500
400
300
200
100
0
0:00
N9 Volga
N9
N5
N11
N13
N10
N7
1:00
Temperature
profile
measured
by MMTP-5
N12
2:00
3:00
4:00
5:00
Time6:00
[hh:mm]
12,13
1,2,3
4
August 6, 2004
August 7, 2004
Stationary MTP-5
Time variation
Space variation
Mobile MTP-5
Particular results of immediate comparisons of Mobile and Stationary devices August 6, 2004
N1
N0
N10
N0
N2
N0
N11
N0
N5
N0
N12
N0
Dependence of correlation coefficient from distance between
stationary and mobile profilers.
Vertical
temperature
gradient g
[degree/100 m]
650
550
450
350
250
600
450
300
150
0
NNNNNNNN
5 799 111 1
0 11( 012 3
: : : V233 4
2 05o: : : :
0 00l 315 3
150
50
N 13 4:30
N 11 3:10
N 9 (Volga) 2:00
N 7 1:00
Altitude [m]
g = (Th+1-Th)*2
-1--0.5
0-0.5
1-1.5
2-2.5
3-3.5
4-4.5
5-5.5
-0.5-0
0.5-1
1.5-2
2.5-3
3.5-4
4.5-5
5.5-6
Temperature
difference [OC]
dT = TMTPM-5-TMTP-5
3.5-4.5
2.5-3.5
1.5-2.5
0.5-1.5
-0.5-0.5
-1.5--0.5
-2.5--1.5
-3.5--2.5
-4.5--3.5
-5.5--4.5
August
Measuring points
Time [hh:mm]
6, 2004
Vertical
temperature
gradient g
[degree/100 m]
650
550
450
350
250
150
-1--0.5
0-0.5
1-1.5
2-2.5
3-3.5
4-4.5
5-5.5
dT = TMMTP-5-TMTP-5
50
3.5-4.5
2.5-3.5
1.5-2.5
0.5-1.5
-0.5-0.5
-1.5--0.5
-2.5--1.5
-3.5--2.5
-4.5--3.5
-5.5--4.5
600
450
300
150
0
NNNNNNNN
5 799 111 1
0 11( 012 3
: : : V233 4
2 05o: : : :
-0.5-0
0.5-1
1.5-2
2.5-3
3.5-4
4.5-5
5.5-6
Temperature
difference [OC]
N 13 4:30
N 11 3:10
N 9 (Volga) 2:00
N 7 1:00
Altitude [m]
g = (Th+1-Th)*2
August 7, 2004
Measuring points
Time [hh:mm]
September 1, 2004
Temperature
profile
measured
by MMTP-5
12,13
1,2,3
4
Vertical
temperature
gradient g
[degree/100 m]
650
550
450
350
250
g = (Th+1-Th)*2
-1--0.5
0-0.5
1-1.5
2-2.5
3-3.5
4-4.5
5-5.5
-0.5-0
0.5-1
1.5-2
2.5-3
3.5-4
4.5-5
5.5-6
Temperature
difference [OC]
150
dT = TMMTP-5-TMTP-5
50
N 13 4:30
N 11 3:10
N 9 (Volga) 2:00
N 7 1:00
Altitude [m]
3.5-4.5
2.5-3.5
1.5-2.5
0.5-1.5
-0.5-0.5
-1.5--0.5
-2.5--1.5
-3.5--2.5
-4.5--3.5
-5.5--4.5
600
450
300
150
0
NNNNNNNN
5 799 111 1
0 11( 012 3
: : : V233 4
2 05o: : : :
September 1, 2004
Measuring points
Time [hh:mm]
October 16-17, 2004
Temperature
profile
measured
by MMTP-5
12,13
1,2,3
4
Vertical
temperature
gradient g
[degree/100 m]
650
550
450
350
250
150
-1--0.5
0-0.5
1-1.5
2-2.5
3-3.5
4-4.5
5-5.5
dT = TMMTP-5-TMTP-5
50
3.5-4.5
2.5-3.5
1.5-2.5
0.5-1.5
-0.5-0.5
-1.5--0.5
-2.5--1.5
-3.5--2.5
-4.5--3.5
-5.5--4.5
600
450
300
150
0
NNNNNNNN
5 799 111 1
0 11( 012 3
: : : V233 4
2 05o: : : :
-0.5-0
0.5-1
1.5-2
2.5-3
3.5-4
4.5-5
5.5-6
Temperature
difference [OC]
N 13 4:30
N 11 3:10
N 9 (Volga) 2:00
N 7 1:00
Altitude [m]
g = (Th+1-Th)*2
October 16-17, 2004
Measuring points
Time [hh:mm]
October 17-18, 2004
Temperature
profile
measured
by MMTP-5
12,13
1,2,3
4
Vertical
temperature
gradient g
[degree/100 m]
650
550
450
350
g = (Th+1-Th)*2
-1--0.5
0-0.5
1-1.5
2-2.5
3-3.5
4-4.5
5-5.5
-0.5-0
0.5-1
1.5-2
2.5-3
3.5-4
4.5-5
5.5-6
250
N 13 4:30
N 11 3:10
Altitude [m] 50
N 9 (Volga) 2:00
N 7 1:00
150
600
450
300
150
0
NNNNNNNN
5 799 111 1
0 11( 012 3
Temperature
difference [OC]
dT = TMMTP-5-TMTP-5
3.5-4.5
2.5-3.5
1.5-2.5
0.5-1.5
-0.5-0.5
-1.5--0.5
-2.5--1.5
-3.5--2.5
-4.5--3.5
-5.5--4.5
October 17-18, 2004
Conclusion
The measurements of temperature stratification in the Nijny-Novgorod
industrial agglomeration carried out by means of mobile (MMTP-5) and stationary
temperature profilers MTP-5 showed:
Mobile measuring temperature profiler MMTP-5 allows to investigate the spatial
variability of atmospheric boundary layer temperature stratification.
In the inspected territory it was observed 3-5 sufficiently well resolved and steady
zones distinguishing by the thermal structure of ABL. These zones are coupled with
the orographical features of the city. The sizes and internal structure of these zones
depended on the synoptic situation.
 The zone of representative using of stationary MTP-5 data for the forecast of bad
weather conditions (BWC) was determined on the basis of data obtained during
these measurements. As consequent from the analysis, the data of stationary MTP-5
can be used regularly in the forecast of BWC within the radius 6-8 km. The
extending of forecast to entire territory on the city and its suburb is possibly only
under the specified synoptic conditions.
Mobile system for atmospheric temperature profile
monitoring: mobile MTP-5
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