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Automatic detection of boundary layer height using Doppler lidar measurements

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HAL Id: meteo-01379589

https://hal-meteofrance.archives-ouvertes.fr/meteo-01379589

Submitted on 11 Oct 2016

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Automatic detection of boundary layer height using Doppler lidar measurements

Thomas Rieutord, W Brewer, R Hardesty

To cite this version:

Thomas Rieutord, W Brewer, R Hardesty. Automatic detection of boundary layer height using Doppler lidar measurements. CIRES rendez-vous 2014, May 2014, Boulder, United States. 2014. �meteo- 01379589�

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6. Results 6. Results

Automatic detection of boundary layer height using Doppler lidar measurements

Thomas A. Rieutord

1

, W. Alan Brewer

2

, R. Mike Hardesty

2,3

1Météo-France, ENM; 2Chemical Sciences Division, NOAA; 3Cooperative Institute for Research in Environmental Sciences

4. Continuity test 4. Continuity test

3. Peak detection method

Idea : BL top is a transition between BL and free atmosphere (FA). We identify peaks in both the turbulence and the gradient of the aerosol backscatter profiles.

3. Peak detection method

Idea : BL top is a transition between BL and free atmosphere (FA). We identify peaks in both the turbulence and the gradient of the aerosol backscatter profiles.

5. Cluster analysis 5. Cluster analysis 1. Theory 1. Theory

2. Data

From campaign : TXFlux – Texas Flux Study Period : Mar, Apr, Oct, 2013

Main goal of the campaign : Study the methane emissions fluxes downwind of oil/gas large fields.

Type of lidar : HRDL – λ=2μm, PRF=200, Data rate=2Hz, Range gate size = 30m.

2. Data

From campaign : TXFlux – Texas Flux Study Period : Mar, Apr, Oct, 2013

Main goal of the campaign : Study the methane emissions fluxes downwind of oil/gas large fields.

Type of lidar : HRDL – λ=2μm, PRF=200, Data rate=2Hz, Range gate size = 30m.

Two types of profile Peaks connected

to the ground

Turbulence must maintain high

values all the way to the ground.

1) Define a peak- based threshold 2) Look for the

highest point above the

threshold

BLH = highest point connected to the ground

Peaks that track a transition

Transitions such as BL top are peaks in gradient of aerosol backscatter profiles.

1) Compute the gradient profile with Haar

wavelet transform

2) Record peaks in gradient profile

For each peak, we look for neighbors in a window of

height and time.

All the peaks in the same window are linked

together by a thread.

Idea : BL air is characterized by - High

turbulence - High aerosol

content

We track the BL air by gathering these high

values in clusters

Purpose

Boundary layer height (BLH) is an essential parameter for air quality research, and forecasting. Doppler lidars provide continuous information such as wind speed and direction, turbulence information and backscatter intensity with high resolution (both spatial and temporal). This work aims to find an algorithm able to automatically detect the BLH using all the lidar-measured variables. Two methods will be presented : one based on peak detection, one based on cluster analysis.

Purpose

Boundary layer height (BLH) is an essential parameter for air quality research, and forecasting. Doppler lidars provide continuous information such as wind speed and direction, turbulence information and backscatter intensity with high resolution (both spatial and temporal). This work aims to find an algorithm able to automatically detect the BLH using all the lidar-measured variables. Two methods will be presented : one based on peak detection, one based on cluster analysis.

6.1 A good day

Transition that human eye identifies as BLH in the data is selected by both methods

6.1 A good day

Transition that human eye identifies as BLH in the data is selected by both methods

7. Conclusion and next steps

At this point, we have an estimation of BLH from each of the data (velocity variance, aerosol backscatter, wind), independently. But each one have its drawback (range, availability, accuracy). Mixing them intelligently could be a way to build a full time available and accurate estimator.

The clustering analysis method mixes the data from the beginning, but not yet the wind info. The main drawback is representativeness of the cluster.

 Add wind information (wind speed and wind direction) in clustering

 Investigate the convergence of the seeds (are the final clusters representative?)

 Improve the mechanism to choose the peaks

 Mix the 6 peak estimators into a single one

 Evaluate the algorithms on a extended dataset

6.2 A bad day

The chosen peak is not the good one, and the cluster analysis doesn’t identify the BL air

6.2 A bad day

The chosen peak is not the good one, and the cluster analysis doesn’t identify the BL air

Algorithm : “K means” (non-hierarchical clustering). Used mainly in data-mining.

From : Toledo et al. (2013)*

Description : Iterative algorithm with three steps in the main loop :

1) Calculate point-to-seed distances.

2) Link each point with its closest seed.

3) Redefine the seed.

Estimator Kmeans VS var VS RCI BT var BT RCI WP spd WP grad

Successful

days 13 (62%) 17 (81%) 9 (43%) 11 (53%) 10 (48%) 13 (62%) 7 (33%)

*Reference : Toledo D. et al. (2013): Cluster analysis: a new approach applied to lidar measurements for atmospheric boundary layer height estimation. J.Atm.Oceanic Tech, 31, 422-436.

VAD scan

Bowtie scan

Vertical staring

We choose among

the peaks with a

continuity test.

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