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Climate Change in the Arctic Ocean NABOS 2013 Atmospheric Boundary Layer (ABL) and Turbulence Tobias Wolf, Nansen Environmental and Remote Sensing Center.

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Presentation on theme: "Climate Change in the Arctic Ocean NABOS 2013 Atmospheric Boundary Layer (ABL) and Turbulence Tobias Wolf, Nansen Environmental and Remote Sensing Center."— Presentation transcript:

1 Climate Change in the Arctic Ocean NABOS 2013 Atmospheric Boundary Layer (ABL) and Turbulence Tobias Wolf, Nansen Environmental and Remote Sensing Center

2 2NABOS 2013 Chapter 1 1. ABL structure, a quick overview 2. Turbulence in the atmosphere and ocean 3. Measuring Temperature Profiles in the ABL 4. MTP-5HE

3 ABL as part of the troposphere 3NABOS 2013 Arya, S., Introduction to Micrometeorology, 2001 (1) ABL structure

4 4 ABL structure over land surfaces in mid-latitudes NABOS 2013 Stull, R.B., An Introduction to Boundary Layer Meteorology, 1997 (1) ABL structure

5 Surface energy balance over land Oke, T.R., Boundary Layer Climates, 1897 NABOS 20135 (1) ABL structure

6 Surface energy balance over water Oke, T.R., Boundary Layer Climates, 1897 NABOS 20136 (1) ABL structure

7 Surface energy balance over snow Oke, T.R., Boundary Layer Climates, 1897 NABOS 20137 (1) ABL structure

8 8NABOS 2013 Chapter 2 1. ABL structure, a quick overview 2. Turbulence in the atmosphere and ocean 3. Measuring Temperature Profiles in the ABL 4. MTP-5HE

9 Dissipation 9 How to make Marie stir my tea Lets assume Marie did not stir a cup but a supercup without friction at the glass. What would be the processes stopping my little tea-twister and how long would that take (the cup is 10 cm in diameter)? (2) Turbulence

10 Kolmogorov theory on turbulent energy cascading Left: Vallis, G.K., Atmospheric and Oceanic Fluid Dynamics, 2006 Right: Grant et al., 1962 Lewis Fry Richardson: Big whirls have little whirls, that feed on their velocity. And little whirls have lesser whirls, and so on to viscosity. (2) Turbulence

11 Modelling techniques Reynolds averaged numerical simulation (RANS) Large Eddy Simulation (LES) Direct Numerical Simulation (DNS) (2) Turbulence

12 12NABOS 2013 Chapter 3 1. ABL structure, a quick overview 2. Turbulence in the atmosphere and ocean 3. Measuring Temperature Profiles in the ABL 4. MTP-5HE

13 13 In-situ techniques Meteorological towers Radiosoundings Teathered Balloons RPAS Measurement stations along the slope of mountains NABOS 2013 (3) Measuring temperature

14 14 Remote Sensing Techniques Sound Detection and Ranging-Radar Acoustic Sounding System (SODAR-RASS) Microwave Temperature Profiler (MTP) NABOS 2013 (3) Measuring temperature

15 1. ABL structure, a quick overview 2. Turbulence in the atmosphere and ocean 3. Measuring Temperature Profiles in the ABL 4. MTP-5HE Chapter 4

16 16 Atttex MTP-5HE 56.7 GHz thermal radiation at side slope of Oxygen absorption band Vertically resolved signal from angular scanning Vertical resolution: 25 m until 100 m and 50 m until 1000 m Temporal resolution: 5 min NABOS 2013 (3) MTP-5HE

17 17 Data Reliability NABOS 2013 Inter-comparison of filtered temperatures at the AMS and MTP- 5HE at the heights of the AMS for |v| > 5 m/s (3) MTP-5HE

18 18 Filtering I NABOS 2013 Esau, Wolf et al., 2013, in print (3) MTP-5HE Inter-comparison of all temperatures at the AMS and MTP-5HE at the heights of the AMS for |v| > 5 m/s

19 19NABOS 2013 Esau, Wolf et al., 2013, in print (3) MTP-5HE Top panel: MTP-5HE measurement during precipitation. Lower panel: rain rate measured with rain radar Filtering II

20 20 Filtering NABOS 2013 What did we use in Bergen? RH from AMS at elevated location and nearby instrument. Rain radar What could you use here? Ceilometer (LIDAR) Radiosoundings Cloud observations (3) MTP-5HE

21 21 Thank you for your attention NABOS 2013


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