Stocktake Sale on now: wide range of books at up to 70% off!
Register      Login
Journal of Southern Hemisphere Earth Systems Science Journal of Southern Hemisphere Earth Systems Science SocietyJournal of Southern Hemisphere Earth Systems Science Society
A journal for meteorology, climate, oceanography, hydrology and space weather focused on the southern hemisphere
RESEARCH ARTICLE (Open Access)

Variation in growing season water balance in central Victoria, Australia, in relation to large-scale climate drivers

Adam John Marshall
+ Author Affiliations
- Author Affiliations

A Federation University (formerly University of Ballarat), Ballarat, Vic., Australia. Email: adjomarshall@gmail.com

Journal of Southern Hemisphere Earth Systems Science 69(1) 131-145 https://doi.org/10.1071/ES19007
Submitted: 23 September 2018  Accepted: 27 May 2019   Published: 11 June 2020

Journal Compilation © BoM 2019 Open Access CC BY-NC-ND

Abstract

The precipitation and evaporation records from 1972 to 2013 were analysed at five stations in central Victoria, Australia. The stations formed a north-south transect of sites across a distinct climatic gradient spanning the dry inland plains, the Great Dividing Range and the southern coastal zone. The focus was on the March–November ‘Growing Season’ when typically higher available moisture is critical for a variety of agricultural practices and water management across the region. Growing season rainfall trends were fairly consistent across all stations with ongoing declines generally observed in all months with the exception of November, with the most notable declines in April, May and October. Pan evaporation recorded display greater variation between stations with both significant positive and negative trends evident within the season across the station network. The influence of El Niño–Southern Oscillation and Indian Ocean Dipole on rainfall and pan evaporation was statistically significant, increasing through winter and peaking in spring at all stations. The Southern Annular Mode displayed marked intraseasonal influence which appeared to be highly location dependent. Interestingly, the tropical climate drivers displayed a stronger relationship with pan evaporation than rainfall over the analysis period. This highlighted the potential benefits of taking a broader terrestrial water balance (TWB) perspective of both pan evaporation and rainfall, a concept previously termed ‘Effective Rainfall’. Critically, this study shows the importance of understanding regional variation in TWB elements with respect to local topography and geographic location, as well as intraseasonal variations within the overall growing season.


References

Ashcroft, L., Karoly, D., and Gergis, J. (2012). Temperature variations of southeastern Australia, 1860–2011. Aust. Meteorol. Oceanogr. J. 62, 227–245.
Temperature variations of southeastern Australia, 1860–2011.Crossref | GoogleScholarGoogle Scholar |

Brown, J. N., McIntosh, P. C., Pook, M. J., and Risbey, J. S. (2009). An investigation of the links between ENSO flavours and rainfall processes in southeastern Australia. Mon. Wea. Rev. 137, 3786–3795.
An investigation of the links between ENSO flavours and rainfall processes in southeastern Australia.Crossref | GoogleScholarGoogle Scholar |

Bureau of Meteorology (BOM) (2006). Special Climate Statement 9 – An exceptionally dry decade in parts of southern and eastern Australia: October 1996 – September 2006. Issued 10th October 2006. pp. 9. (National Climate Centre.) Available at http://www.bom.gov.au/climate/current/statements/scs9a.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) and CSIRO (2012). State of the Climate 2012. 12 pp. Available at http://www.bom.gov.au/announcements/media_releases/ho/stateClimate2012.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) (2013a). Basic Climatological Station Metadata: Cairn Curran 088009. Available at http://www.bom.gov.au/clim_data/cdio/metadata/pdf/siteinfo/IDCJMD0040.088009.SiteInfo.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) (2013b). Basic Climatological Station Metadata: Malmsbury 088042. Available at http://www.bom.gov.au/clim_data/cdio/metadata/pdf/siteinfo/IDCJMD0040.088042.SiteInfo.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) (2013c). Basic Climatological Station Metadata: Moorabool Reservoir 087045. Available at http://www.bom.gov.au/clim_data/cdio/metadata/pdf/siteinfo/IDCJMD0040.087045.SiteInfo.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) (2013d). Basic Climatological Station Metadata: White Swan Reservoir 089048. Available at http://www.bom.gov.au/clim_data/cdio/metadata/pdf/siteinfo/IDCJMD0040.089048.SiteInfo.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) (2013e). Basic Climatological Station Metadata: Durdidwarrah 087021. Available at http://www.bom.gov.au/clim_data/cdio/metadata/pdf/siteinfo/IDCJMD0040.087021.SiteInfo.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) (2013f). Basic Climatological Station Metadata: Geelong Salines 087023. Available at http://www.bom.gov.au/clim_data/cdio/metadata/pdf/siteinfo/IDCJMD0040.087023.SiteInfo.pdf [Verified 22 April 2020].

Bureau of Meteorology (BOM) (2013g). Basic Climatological Station Metadata: Wurdiboluc Reservoir 087126. Available at http://www.bom.gov.au/clim_data/cdio/metadata/pdf/siteinfo/IDCJMD0040.087126.SiteInfo.pdf [Verified 22 April 2020].

Cai, W., Rensch, P. V., and Cowan, T. (2011). Influence of global-scale variability on the subtropical ridge over Southeast Australia. J. Clim. 24, 6035–6053.
Influence of global-scale variability on the subtropical ridge over Southeast Australia.Crossref | GoogleScholarGoogle Scholar |

Cai, W., Cowan, T., and Thatcher, M. (2012). Rainfall reductions over southern hemisphere semi-arid regions: the role of subtropical dry zone expansion. Sci. Rep. 2, 1–5.
Rainfall reductions over southern hemisphere semi-arid regions: the role of subtropical dry zone expansion.Crossref | GoogleScholarGoogle Scholar |

Cai, W., and Cowan, T. (2013). Southeast Australia autumn rainfall reduction: a climate-change-induced poleward shift of ocean–atmosphere circulation. J. Clim. 26, 189–205.
Southeast Australia autumn rainfall reduction: a climate-change-induced poleward shift of ocean–atmosphere circulation.Crossref | GoogleScholarGoogle Scholar |

Fu, G., Charles, S. P., and Yu, J. (2009). A critical overview of pan evaporation trends over the last 50 years. Clim. Change 97, 193–214.
A critical overview of pan evaporation trends over the last 50 years.Crossref | GoogleScholarGoogle Scholar |

Hendon, H. H., Thompson, D. W. J., and Wheeler, M. C. (2007). Australian rainfall and surface temperature variations associated with the southern hemisphere annular mode. J. Clim. 20, 2452–2467.
Australian rainfall and surface temperature variations associated with the southern hemisphere annular mode.Crossref | GoogleScholarGoogle Scholar |

Ho, M., Kiem, A. S., and Verdon-Kidd, D. C. (2012). The southern annular mode: a comparison of indices. Hydrol. Earth Syst. Sci. 16, 967–982.
The southern annular mode: a comparison of indices.Crossref | GoogleScholarGoogle Scholar |

Hobbins, M. T., Dai, A., Roderick, M. L., and Farquhar, G. D. (2008). Revisiting the parameterization of potential evaporation as a driver of long-term water balance trends. Geophys. Res. Lett. 35, 1–6.
Revisiting the parameterization of potential evaporation as a driver of long-term water balance trends.Crossref | GoogleScholarGoogle Scholar |

Johnson, F., and Sharma, A. (2010). A comparison of Australian open water body evaporation trends for current and future climates estimated from Class A evaporation pans and general circulation models. J. Hydrometeorol. 11, 105–121.
A comparison of Australian open water body evaporation trends for current and future climates estimated from Class A evaporation pans and general circulation models.Crossref | GoogleScholarGoogle Scholar |

Jovanovic, B., Jones, D. A., and Collins, D. (2008). A high quality monthly pan evaporation dataset for Australia. Clim. Change 87, 517–535.
A high quality monthly pan evaporation dataset for Australia.Crossref | GoogleScholarGoogle Scholar |

Kiem, A. S., and Verdon-Kidd, D. C. (2010). Towards understanding hydroclimatic change in Victoria, Australia – preliminary insights into the “Big Dry”. Hydrol. Earth Syst. Sci. 14, 433–445.
Towards understanding hydroclimatic change in Victoria, Australia – preliminary insights into the “Big Dry”.Crossref | GoogleScholarGoogle Scholar |

Marshall, A. J. (2016). Precipitation and evaporative aspects of the terrestrial water balance in Central Victoria and their relationship to large-scale climate drivers during the growing season. Masters Thesis, University of Ballarat/Federation University, Australia. Available at https://researchonline.federation.edu.au/vital/access/manager/Repository/vital:10828 [Verified 22 April 2020].

Meneghini, B., Simmonds, I., and Smith, I. N. (2007). Association between Australian rainfall and the Southern Annular Mode. Int. J. Climatol. 27, 109–121.
Association between Australian rainfall and the Southern Annular Mode.Crossref | GoogleScholarGoogle Scholar |

Meyers, G., McIntosh, P., Pigot, L., and Pook, M. (2007). The years of El Niño, La Niña and interaction with the Indian Ocean. J. Clim. 20, 2872–2880.
The years of El Niño, La Niña and interaction with the Indian Ocean.Crossref | GoogleScholarGoogle Scholar |

Murphy, B. F., and Timbal, B. (2008). A review of recent climate variability and climate change in southeastern Australia. Int. J. Climatol. 28, 859–879.
A review of recent climate variability and climate change in southeastern Australia.Crossref | GoogleScholarGoogle Scholar |

Nicholls, N. (2004). The changing nature of Australian droughts. Clim. Change 63, 323–336.
The changing nature of Australian droughts.Crossref | GoogleScholarGoogle Scholar |

Power, S., Haylock, M., Colman, R., and Wang, X. (2006). The predictability of interdecadal changes in ENSO activity and ENSO teleconnections. J. Clim. 19, 4755–4771.
The predictability of interdecadal changes in ENSO activity and ENSO teleconnections.Crossref | GoogleScholarGoogle Scholar |

Rancic, A., Salas, G., Kathuria, A., Acworth, I., Johnston, W., Smithson, A., and Beale, G. (2009). Climatic influence on shallow fractured-rock groundwater systems in the Murray–Darling Basin, NSW. (NSW Department of Environment and Climate Change.) Available at http://www.environment.nsw.gov.au/resources/salinity/09108groundwatermdb.pdf [Verified 22 April 2020].

Rayner, D. P. (2005). Australian synthetic daily Class A pan evaporation – technical report December 2005. (Queensland Department of Natural Resources and Mines.) Available at https://www.longpaddock.qld.gov.au/silo/documentation/AustralianSyntheticDailyClassAPanEvaporation.pdf [Verified 22 April 2020].

Rayner, D. P. (2007). Wind run changes: the dominant factor affecting pan evaporation trends in Australia. J. Clim. 20, 3379–3394.
Wind run changes: the dominant factor affecting pan evaporation trends in Australia.Crossref | GoogleScholarGoogle Scholar |

Risbey, J. S., Pook, M. J., McIntosh, P. C., Wheeler, M. C., and Hendon, H. H. (2009). On the remote drivers of rainfall variability in Australia. Mon. Wea. Rev. 137, 3233–3253.
On the remote drivers of rainfall variability in Australia.Crossref | GoogleScholarGoogle Scholar |

Roderick, M. L., and Farquhar, G. D. (2002). The cause of decreased pan evaporation over the past 50 years. Sci. Mag. 298, 1410–1411.
The cause of decreased pan evaporation over the past 50 years.Crossref | GoogleScholarGoogle Scholar |

Roderick, M. L., and Farquhar, G. D. (2004). Changes in Australian pan evaporation from 1970 to 2002. Int. J. Climatol. 24, 1077–1090.
Changes in Australian pan evaporation from 1970 to 2002.Crossref | GoogleScholarGoogle Scholar |

Roderick, M. L., Rotstayn, L. D., Farquhar, G. D., and Hobbins, M. T. (2007). On the attribution of changing pan evaporation. Geophys. Res. Lett. 34, 1–6.
On the attribution of changing pan evaporation.Crossref | GoogleScholarGoogle Scholar |

Roderick, M. L., Hobbins, M. T., and Farquhar, G. D. (2009a). Pan evaporation trends and the terrestrial water balance. I. Principles and observations. Geogr. Compass 3/2, 746–760.
Pan evaporation trends and the terrestrial water balance. I. Principles and observations.Crossref | GoogleScholarGoogle Scholar |

Roderick, M. L., Hobbins, M. T., and Farquhar, G. D. (2009b). Pan evaporation trends and the terrestrial water balance. II. Energy balance and interpretation. Geogr. Compass 3/2, 761–780.
Pan evaporation trends and the terrestrial water balance. II. Energy balance and interpretation.Crossref | GoogleScholarGoogle Scholar |

Saji, N. H., Goswami, B. N., Vinayachandran, P. N., and Yamagata, T. (1999). A dipole mode in the tropical Indian Ocean. Nature 401, 360–363.
A dipole mode in the tropical Indian Ocean.Crossref | GoogleScholarGoogle Scholar |

Timbal, B., Arblaster, J., Braganza, K., Fernandez, E., Hendon, H., Murphy, B., Raupach, M., Rakich, C., Smith, I., Whan, K., and Wheeler, M. (2010). Understanding the anthropogenic nature of the observed rainfall decline across South Eastern Australia. CAWCR technical report no. 026. Available at http://www.cawcr.gov.au/publications/technicalreports/CTR_026.pdf [Verified 22 April 2020].

Timbal, B., and Fawcett, R. (2012). A historical perspective on southeastern Australian Rainfall since 1865 using the instrumental record. J. Clim. 26, 1112–1129.
A historical perspective on southeastern Australian Rainfall since 1865 using the instrumental record.Crossref | GoogleScholarGoogle Scholar |

Trewin, B., and Vermont, H. (2010). Changes in the frequency of record temperatures in Australia, 1957–2009. Aust. Meteorol. Oceanogr. J. 60, 113–119.
Changes in the frequency of record temperatures in Australia, 1957–2009.Crossref | GoogleScholarGoogle Scholar |

Ummenhofer, C. C., England, M. H., McIntosh, P. C., Meyers, G. A., Pook, M. J., Risbey, J. S., Sen Gupta, A., and Taschetto, A. S. (2009). What causes southeast Australia’s worst droughts? Geophys. Res. Lett. 36, 1–5.
What causes southeast Australia’s worst droughts?Crossref | GoogleScholarGoogle Scholar |

Ummenhofer, C. C., Sen Gupta, A., Briggs, P. R., England, M. H., McIntosh, P. C., Meyers, G. A., Pook, M. J., Raupach, M. R., and Risbey, J. S. (2010). Indian and Pacific Ocean influences on southeast Australian drought and soil moisture. J. Clim. 24, 1313–1336.
Indian and Pacific Ocean influences on southeast Australian drought and soil moisture.Crossref | GoogleScholarGoogle Scholar |

van Dijk, M. H. (1985). Reduction in evaporation due to the bird screen used in the Australian class A pan evaporation network. Austr. Meteorol. Mag. 33, 181–183.

Verdon-Kidd, D. C., and Kiem, A. S. (2009a). Nature and causes of protracted droughts in southeast Australia: comparison between the Federation, WWII, and Big Dry droughts. Geophys. Res. Lett. 36, L22707.
Nature and causes of protracted droughts in southeast Australia: comparison between the Federation, WWII, and Big Dry droughts.Crossref | GoogleScholarGoogle Scholar |

Verdon-Kidd, D. C., and Kiem, A. S. (2009b). On the relationship between large-scale climate modes and regional synoptic patterns that drive Victorian rainfall. Hydrol. Earth. Syst. Sci. 13, 467–479.
On the relationship between large-scale climate modes and regional synoptic patterns that drive Victorian rainfall.Crossref | GoogleScholarGoogle Scholar |

Verdon-Kidd, D. C., Kiem, A. S., and Moran, R. (2014). Links between the Big Dry in Australia and hemispheric multi-decadal climate variability. Hydrol. Earth. Syst. Sci. 18, 2235–2256.
Links between the Big Dry in Australia and hemispheric multi-decadal climate variability.Crossref | GoogleScholarGoogle Scholar |

Whan, K., Bertrand Timbal, B., and Lindesay, J. (2013). Linear and nonlinear statistical analysis of the impact of sub-tropical ridge intensity and position on south-east Australian rainfall. Int. J. Climatol. 34, 326–342.
Linear and nonlinear statistical analysis of the impact of sub-tropical ridge intensity and position on south-east Australian rainfall.Crossref | GoogleScholarGoogle Scholar |