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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Analysis of katabatic flow using infrared imaging at micro and meso scale
Martina Grudzielanek Jan Cermak Department of Geography Ruhr-Universität Bochum; Climatology Roland Vogt University of Basel; Meteorology, Clomatology, Remote Sensing
[email protected] www.climate.rub.de
AMS - Boundary Layer and Turbulences 06/10/2014
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Infrared imaging at micro scale
Adapted from BENDIX 2004
Kaltluft-See
Cold air drops
1
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Experimental setup
Setup design on sloping grassland Infrared-Camera: VarioCam
384x288 IR pixel; 7,5 – 14 μm
Evaluation of the Infrared (IR) method by cross-correlation of Infrared temperatures and sensor temperatures at almost identical locations
- micro scale -
2
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Special feature: identifiication of new and only supposed phenomena
Cold air drop with turbulences
- micro scale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
IR data analysis Observation of near ground inversion in time response
Hovmöller diagram for IR_Profil1 for two hours of measurement at cold air flow phase
hei
ght
ove
r gr
ou
nd
[cm
]
IR t
emp
erat
ure
[°C
]
time [hours]
Analysis as: - visualization - statistical time series analysis
- micro scale -
4
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
8 Hovmöller diagram for exemplary 10 minutes at cold air flow phase
hei
ght
ove
r gr
ou
nd
[cm
]
hei
ght
ove
r gr
ou
nd
[IR
-Pix
el]
IR t
emp
erat
ure
[°C
]
IR temperature [°C] cold air drop peak
time [hours]
Observation of passing cold air drops and analysis of their vertical temperature gradients
Classification of cold air drops in different types based on size, period, frequency and vertical temperature gradient is possible!
- micro scale -
5
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
METCRAX II - The Meteor Crater Experiment II http://www.inscc.utah.edu/~whiteman/metcrax2/
Barringer Meteor Crater, Arizona: meteorological measurements in Oct. 2013 cold air flow into the crater Dynamic processes in and around the
crater
Dave Whiteman (PI, University of Utah) and Team of international scientists
Infrared imaging at meso scale
5 Infrared Cameras: VarioCams; 7,5 – 14 μm
384x288 IR pixel, 640 x 480 IR pixel
1022 x 766 IR-Pixel
Thanks for technical support and additional IR cameras to Matthias Krauß (InfraTec), Andrea Pitacco (University of Padova and Christian Bernhofer (University of Dresden).
6
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale - meso scale -
7
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Exemplary research questions at METCRAX II, wich are additionally analysed with the IR method:
1. Identification and dynamics of the cold and warm air inflow into the craters south rim
2. Thickness of the cold air pool in the crater over the night and at special flow dynamic situations
3. Warm air intrusion (WAI) and resulting turbulences at the craters ground WAI
Cold air pool
- meso scale -
8
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Turbulence in the crater, no steady inversion
- meso scale -
9
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Warm Air Intrusion at stable inversion at 10/22/2013 from 3 to 4 UTC
- meso scale -
10
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
IR profile and Infrared profile diagram for the animated period
- meso scale -
11
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
IR method for the analysis of dynamic air processes like catabatic flows
What is possible? - Analysis of air mass processes, which are attended by air temperature changes - Analysis in different scales - data collection as time sequenced IR data - Combination with other data are possible - Data analysis as
1. visualisation 2. time series statistical analysis
What has to be considered? - The recorded surfaces have to be dry and temperatur reactive the surface has to react fast with air temperature changes
- surface properties can be different in one recorded IR investigation area emissivity, angle of IR Cam view, humidity (near ground condensation), temperature reactivity and heat storage
- …
Big benefit for dynamic air process understanding by additional IR method
12
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Classification of cold air drops in different types based on: - size - period - frequency - … - vertical temperature gradient:
Hö
he
Hö
he
temperature
1
temperature
2
temperature
3
temperature
4
hei
ght
hei
ght
hei
ght
hei
ght
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layer and Turbulences 10/06/2014
Analysis of katabatic flow using infrared imaging at micro and meso scale
Hovmöller diagram for an exemplary cold air drop passing the projection screen
IR t
emp
erat
ure
[°C
]
hei
ght
ove
r gr
ou
nd
[cm
]
hei
ght
ove
r gr
ou
nd
[IR
-Pix
el]
IR temperature [°C] cold air drop moments
maximum of cold air drop
time [hours]
Observation of individual passing cold air drops in time response