Analysis of katabatic flow using infrared imaging at micro...
Transcript of Analysis of katabatic flow using infrared imaging at micro...
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Martina Grudzielanek Jan Cermak Ruhr-Universität Bochum, Germany Roland Vogt University of Basel, Switzerland
[email protected] www.climate.rub.de
AMS - Boundary Layers and Turbulence 06/10/2014
Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Infrared imaging at microscale
Adapted from BENDIX 2004
Cold air pool
Cold air drops
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
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
- microscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Special feature: identification of new and only supposed phenomena
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale - microscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
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
- microscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
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 -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
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).
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale - mesoscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Exemplary research questions at METCRAX II, which are additionally analyzed with the IR method:
1. Identification and dynamics of the cold and warm air inflow into the crater´s south rim
2. Thickness of the cold air pool in the crater over the night and at special flow situations
3. Warm air intrusion (WAI) and resulting turbulence at the crater´s ground WAI
Cold air pool
- mesoscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Turbulence in the crater, no steady inversion
- mesoscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Warm Air Intrusion at stable inversion at 10/22/2013 from 3 to 4 UTC
- mesoscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
IR profile and Infrared profile diagram for the animated period
- mesoscale -
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Conclusions: 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. visualization 2. time series statistical analysis
What has to be considered? - The recorded surfaces have fit in order to heat capacity and thermal conductivity 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 understanding dynamic air processes by additional IR method
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Martina Grudzielanek, Roland Vogt, Jan Cermak | [email protected] | www.climate.rub.de | AMS - Boundary Layers and Turbulence 10/06/2014
Analysis of katabatic flow using infrared imaging at micro- and mesoscale
Thanks for your attention!
Sunrise after a really cold night