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Lower atmospheric drying, stability, and increased wildfire activity

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Presentation on theme: "Lower atmospheric drying, stability, and increased wildfire activity"— Presentation transcript:

1 Lower atmospheric drying, stability, and increased wildfire activity
Graham Mills Bureau of Meteorology Research Centre

2 Outline Massive drying was observed at screen level during two major recent fires in Australia - Canberra - 18 January Eyre Peninsula - 11 January 2005 Why? Was this that unusual? How? Predictability?

3 Locality map #1

4 Canberra 18 January 2003 (Mills, 2005, AMM)

5 Meteorological Context

6 Dewpoint

7 The northern dry band? GMS-5 Water Vapour Imagery
3-hourly intervals from 2030 UTC (~ 0500 LDST) (first surface dewpoint drop ~ 0300 UTC)

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13 Eyre Peninsula 11 January 2005

14 Meteorological context

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21 Strong association with 300 hPa IPV

22 A general study? (encouraged by Potter, McCaw)
Stations spread across the southern fire-vulnerable regions Td < -5C (want low moisture content, not just relative humidity) to fire seasons (limit of half-hourly data archive) WV imagery? - Front? - Dynamics?

23 Localities

24 So far……

25 How does dewpoint change?
Moisture equation: - Horizontal advection - Vertical advection - Diabatic processes: - evaporation - turbulent mixing

26 Early results? 68% have WV dry slot VERY evident
67% have front/trough passage - can be pre- or post-frontal Climate control - marked interannual variability - dry soil > deeper mixed layers? OR wet soil > shallow inversion? Daytime mixing - majority occur during day Coastal marine layer erosion (YPLC) Topographic interactions

27 High topography – lowering inversion overnight (Cabramurra)

28 Major circulation changes: Richmond – 2001-2002 fires

29 THEN - Upper tropospheric dry air – how does it reach the surface?
There’s usually a deep mixed layer, so maybe it doesn’t need a lot of help

30 Processes? Upper-jet circulations > dry intrusions
Mixing by cross-frontal circulations - surface-based fronts - mid-tropo. fronts / sloping b-l “lid” Destabilisation by dry-slot (low e) air - (cf Haines Index concepts) Positive feedbacks between upper IPV and lower frontal circulations? ……………?

31 Where next? Monitoring WV imagery an immediate (fire) forecast /weather watch component Complete station analysis and categorise What are the dynamic controls on these events? NWP model predictability (process good, results poor?) Link to fuel moisture models


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