Abstract

The requirement for irrigation water would be affected by the variation of meteorological effects under the conditions of climate change, and irrigation water will always be the major portion of the water consumption in Taiwan. This study tries to assess the impact on irrigation water by climate change in Taoyuan in northern Taiwan. Projected rainfall and temperature during 2046–2065 are adopted from five downscaled general circulation models. The future evapotranspiration is derived from the Hamon method and corrected with the quadrant transformation method. Based on the projections and a water balance model in paddy fields, the future crop water requirement, effective rainfall and the demand for water for irrigation can be calculated. A comparison between the present (2004–2011) and the future (2046–2065) clearly shows that climate change would lead both rainfall and the temperature to rise; this would cause effective rainfall and crop water requirement to increase during cropping seasons in the future. Overall, growing effective rainfall neutralizes increasing crop water requirement, the difference of average irrigation water requirement between the present and future is insignificant (<2.5%). However, based on a five year return period, the future irrigation requirement is 7.1% more than the present in the first cropping season, but it is insignificantly less (2.1%) than the present in the second cropping season.

Highlights

  • The fourth assessment report of the Intergovernmental Panel on Climate Change indicates that the observations of global average temperature during 1995–2006 have increased, and heavy rainfall events have become much frequent

  • The projected rainfall and temperature under climate change in the period of 2046–2065 came from five General circulation models (GCMs): CGCm3 from the Canadian Center for Climate Modeling and Analysis (CCCma), Cm3 from the Center National de Recherches Meteorologiques (CNRM), Mk3.0 from Australia’s

  • This study investigates the impact on the irrigation water requirement under climate change between the present (2004–2011) and future (2046–2065)

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Summary

Introduction

The fourth assessment report of the Intergovernmental Panel on Climate Change indicates that the observations of global average temperature during 1995–2006 have increased, and heavy rainfall events have become much frequent. This report predicts the global average surface temperature during 2080–2099 may rise between 1.1 °C and 6.4 °C more than the period during 1980–1999, and cause crop productivity to increase [1] It clearly shows the affection of climate change. There are many methods to determine the irrigation water requirement, for example: the Erosion Productivity Impact Calculator [8,9], the Global Irrigation Model [10,11], the CROPWAT model [12,13], and the Stochastic Crop Water Production Functions [14] The basis of these models is to capture the characteristics of crop water consumption in different periods.

Materials and Method
Study Area
Projected Rainfall and Temperature
Paddy Water Requirement
FAO Penman-Monteith Equation
Hamon Method
Bias Correction
Calculation of Irrigation Water Requirement
Result and Discussion
Result of Bias Correction
Comparison of Model Estimation and Actual Investigation
Projected Evapotranspiration Analysis
Crop Water Requirement Analysis
Projected Rainfall Analysis
Effective Rainfall Analysis
Findings
Irrigation Water Requirement Analysis
Conclusions
Full Text
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