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.
Download ReportTranscript 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 Thanks a lot for Your Attention! THE END