Channelling flows in the Hunter Valley
Christopher Webb A and Jiwon Park B *A Formerly at Williamtown Weather Services Office, Bureau of Meteorology.
B NSW and ACT Decision Support Service, Bureau of Meteorology, Sydney, NSW, Australia.
Journal of Southern Hemisphere Earth Systems Science 73(2) 194-211 https://doi.org/10.1071/ES22021
Submitted: 17 July 2022 Accepted: 19 July 2023 Published: 1 August 2023
© 2023 The Author(s) (or their employer(s)). Published by CSIRO Publishing on behalf of the Bureau of Meteorology. This is an open access article distributed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License (CC BY-NC-ND)
Abstract
The Hunter Valley is well known for the strong westerly winds in winter and elevated fire danger arising from hot and dry north-westerly winds in summer. These hazards are closely related to the valley channelling in the region, and the connection between the two has been an interest to weather forecasters, emergency service personnel, and the aviation industry. In this paper, the climatology of valley winds is constructed to identify the dominant types of channelling in the Hunter Valley and their preferred directions using the 10-year data of Automatic Weather Station observations, upper air sounding and ERA5 reanalysis data between July 2010 and June 2020. Particular attention is given to the conceptual model of pressure-driven channelling of westerlies in winter and its mechanics, as the climatology shows that it is the main cause of wind-warning conditions in the Hunter.
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References
Australian Institute for Disaster Resilience (2017) ‘Major Incidents of the year 2016–2017’. (AIDR)Ball FK (1956) The theory of strong katabatic winds. Australian Journal of Physics 9, 373–386.
| The theory of strong katabatic winds.Crossref | GoogleScholarGoogle Scholar |
Bureau of Meteorology NSW Regional Office (2007) About East Coast Lows. Available at http://www.bom.gov.au/nsw/sevwx/facts/ecl.shtml
Callaghan J (2021) East coast lows and extratropical transition of tropical cyclones, structures producing severe events and their comparison with mature tropical cyclones. Journal of Southern Hemisphere Earth Systems Science 71, 229–265.
| East coast lows and extratropical transition of tropical cyclones, structures producing severe events and their comparison with mature tropical cyclones.Crossref | GoogleScholarGoogle Scholar |
Carrera ML, Gyakum JR, Lin CA (2009) Observational study of wind channeling within the St Lawrence River Valley. Journal of Applied Meteorology and Climatology 48, 2341–2361.
| Observational study of wind channeling within the St Lawrence River Valley.Crossref | GoogleScholarGoogle Scholar |
Grace W, Holton I (1988) A mechanism for downslope winds with special reference to the Adelaide Gully winds. Meteorological Note 179, Bureau of Meteorology.
Gross G, Wippermann F (1987) Channeling and countercurrent in the Upper Rhine Valley: numerical simulations. Journal of Applied Meteorology and Climatology. 26, 1293–1304.
| Channeling and countercurrent in the Upper Rhine Valley: numerical simulations.Crossref | GoogleScholarGoogle Scholar |
Hersbach H, Bell B, Berrisford P, et al. (2020) The ERA5 global reanalysis. Quarterly Journal of the Royal Meteorological Society 146, 1999–2049.
| The ERA5 global reanalysis.Crossref | GoogleScholarGoogle Scholar |
Manins PC, Sawford BL (1979) A model of katabatic winds. Journal of Atmospheric Sciences 36, 619–630.
| A model of katabatic winds.Crossref | GoogleScholarGoogle Scholar |
Matthews C, Lawrence S, Jardine R, Webb C (2002) Fog forecasting at Sydney Airport. In ‘2002 Weather Services Scientific Conference: extended abstracts’, 3 June–7 June 2002. pp. 58–59. (Bureau of Meteorology, Service Branch)
Muñoz Sabater J (2019) ERA5 hourly data on pressure levels from 1981 to present. (Copernicus Climate Change Service, C3S, and Climate Data Store, CDS) Available at https://www.ecmwf.int/en/forecasts/datasets/reanalysis-datasets/era5 [Verified 2 July 2020]
Weber RO, Kaufmann P (1998) Relationship of synoptic winds and complex terrain flows during the MISTRAL field experiment. Journal of Applied Meteorology. 37, 1486–1496.
| Relationship of synoptic winds and complex terrain flows during the MISTRAL field experiment.Crossref | GoogleScholarGoogle Scholar |
Whiteman CD, Doran JC (1993) The relationship between overlying synoptic-scale flows and winds within a valley. Journal of Applied Meteorology 32, 1669–1682.
| The relationship between overlying synoptic-scale flows and winds within a valley.Crossref | GoogleScholarGoogle Scholar |
Wippermann F (1984) Air flow over and in broad valleys: channeling and coutner-current. Beitraege zur Physik der Atmosphaere 57, 92–105.
World Meteorological Organization (2021) Chapter 1. Annex1.A. Operational measurement uncertainty requirements and instrument performance requirements. In ‘Guide to Instruments and Methods of Observation, Vol. 1. Measurement of Meteorological Variables’. pp. 25–34. (WMO) Available at https://library.wmo.int/doc_num.php?explnum_id=11612
Zhong S, Li J, Whiteman CD, Bian X, Yao W (2008) Climatology of high wind events in the Owen Valley, California. Monthly Weather Review 136, 3536–3552.
| Climatology of high wind events in the Owen Valley, California.Crossref | GoogleScholarGoogle Scholar |