Comparison of latent heat flux estimates over Australia.
McCabe, M.F., Y.Y. Liu, R. Vinukollu, H. Su, J.P. Evans and E.F. Wood
In Anderssen, R.S., R.D. Braddock and L.T.H. Newham (eds) 18th World IMACS Congress and MODSIM09 International Congress on Modelling and Simulation. Modelling and Simulation Society of Australia and New Zealand and International Association for Mathematics and Computers in Simulation, July 2009, pp. 2805-2811. ISBN: 978-0-9758400-7-8.
Documenting the water cycle through modelling and observation is needed for more
fundamental understanding of water exchanges in Earth’s coupled systems. Spatially and temporally
consistent characterization of the hydrological cycle has been a research goal of numerous investigations for
many years. Recent applications of sophisticated modelling approaches has seen the development of a
number of continental and global scale land surface schemes designed for this purpose, providing insight into
the movement of water through the terrestrial system. The Global Land Data Assimilation System (GLDAS)
is one such programme that has delivered significant insights into water and energy exchange over the
Earth’s terrestrial surfaces. While there are a number of numerical modelling based approaches that seek to
describe terrestrial water and energy cycles, an operational, observationally based and temporally consistent
data set for continental scale evapotranspiration is not currently available. As a result, important insights
available from such data do not contribute to model assessment and calibration.
This study compares latent heat fluxes derived from two land surface models, which have been run over
Australia for a 2 year period, with satellite observations and in-situ rainfall measurements. The two land
surface models, component schemes of the Global Land Data Assimilation System, are evaluated against a
newly developed remote sensing based flux dataset, to identify their degree of hydrological coherence. The
remote sensing product utilizes multiple satellite sensors onboard NASA’s Aqua satellite to estimate
instantaneous heat fluxes at the time of satellite overpass, providing an unprecedented spatial coverage of
continental scale evaporation over Australia. An assessment of the agreement between these distinct data sets
is undertaken, with a focus on the reproduction of spatial and temporal patterns of latent heat flux over
portions of the Australian continent.
Figure 2: CLM, NOAH and SEBS output of latent heat flux for three unique 7-day events during 2006
compared with cumulative rainfall determined from gauge data (courtesy of Bureau of Meteorology) for the
same period. Colour bar represents the latent heat flux.
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Last updated 31st January 2013