PENMAN-MONTEITH, FAO-24 REFERENCE CROP EVAPOTRANSPIRATION AND CLASS-APAN DATA IN AUSTRALIA

Citation
Fhs. Chiew et al., PENMAN-MONTEITH, FAO-24 REFERENCE CROP EVAPOTRANSPIRATION AND CLASS-APAN DATA IN AUSTRALIA, Agricultural water management, 28(1), 1995, pp. 9-21
Citations number
3
Categorie Soggetti
Water Resources",Agriculture
ISSN journal
03783774
Volume
28
Issue
1
Year of publication
1995
Pages
9 - 21
Database
ISI
SICI code
0378-3774(1995)28:1<9:PFRCEA>2.0.ZU;2-R
Abstract
The Food and Agriculture Organisation (FAG) methods are recognised as the international standard for estimating reference crop evapotranspir ation (ET(o)). The Penman-Monteith method is currently favoured by the FAO over the FAO-24 methods. The FAO also recommends alternative meth ods which may be used where there are limited data. In this paper, ET( o) estimated using the Penman-Monteith and FAO-24 methods and class-A pan data for 16 Australian locations with a wide range of climate cond itions are compared. The analyses indicate that the FAO-24 Penman ET(o ) estimates are generally 20 to 40% higher than the Penman-Monteith es timates. However, the FAO-24 Radiation and Penman-Monteith methods giv e similar daily ET(o) estimates, Unlike Penman-Monteith, which also re quires windspeed data, the FAO-24 Radiation method estimates ET(o) fro m temperature and sunshine hours, climate variables which are relative ly conservative in space. The FAO-24 Radiation method can thus be used as a surrogate for Penman-Monteith to estimate daily ET(o) for areas where windspeed data are not available. The FAO-24 Blaney-Criddle meth od, which uses only temperature data, gives similar monthly ET(o) esti mates as Penman-Monteith, and is therefore adequate for applications w here only long-term ET(o) estimates are required. The comparisons also show that there is a satisfactory correlation between class-A pan dat a and Penman-Monteith ET(o) for evaporation totals over 3 or more days . However, the pan coefficient is very dependent on local climate and physical conditions, and it should be determined by comparing the pan data with either the Penman-Monteith or FAO-24 Radiation ET(o) estimat es.