4.7 Article

Methodology to assess the changing risk of yield failure due to heat and drought stress under climate change

期刊

ENVIRONMENTAL RESEARCH LETTERS
卷 16, 期 10, 页码 -

出版社

IOP Publishing Ltd
DOI: 10.1088/1748-9326/ac2196

关键词

climate risk assessment; climate change impact; wheat; maize; crop model; relative distribution

资金

  1. International Wheat Yield Partnership [IWYP115]
  2. FACCE JPI MACSUR project through the German Federal Ministry of Food and Agriculture [2815ERA01J]
  3. FACCE MACSUR project by Innovation Fund Denmark
  4. Biotechnology and Biological Sciences Research Council (BBSRC) through Designing Future Wheat [BB/P016855/1]
  5. FACCE JPI MACSUR project through the metaprogram Adaptation of Agriculture and Forests to Climate Change (AAFCC) of the Franch National Research Institute for Agriculture, Food and Environment (INRAE) [031A103B]
  6. German Federal Ministry of Food and Agriculture (BMEL) through the Federal Office for Agriculture and Food (BLE) [2851ERA01J]
  7. German Research Foundation under Germany's Excellence Strategy [EXC-2070-390732324-PhenoRob]
  8. Biotechnology and Biological Sciences Research Council (BBSRC) through Achieving Sustainable Agricultural Systems [NE/N018125/1]
  9. SustES project-Adaptation strategies for sustainable ecosystem services and food security under adverse environmental conditions [CZ.02.1.01/0.0/0.0/16_019/0000797]
  10. BBSRC [BBS/E/C/000I0220] Funding Source: UKRI

向作者/读者索取更多资源

This study utilizes the relative distribution method to assess the risk of yield failure due to heat and drought stress under climate change for rainfed wheat and grain maize in Europe. Results show that climate change leads to shorter return periods of yield failures for maize, with a shift towards lower values in the yield distribution and a reduced frequency of high yields. Conversely, for wheat, yield failures are projected to become less frequent under future scenarios, with a shift towards higher values in the yield distribution and an increase in the frequency of extreme yields.
While the understanding of average impacts of climate change on crop yields is improving, few assessments have quantified expected impacts on yield distributions and the risk of yield failures. Here we present the relative distribution as a method to assess how the risk of yield failure due to heat and drought stress (measured in terms of return period between yields falling 15% below previous five year Olympic average yield) responds to changes of the underlying yield distributions under climate change. Relative distributions are used to capture differences in the entire yield distribution between baseline and climate change scenarios, and to further decompose them into changes in the location and shape of the distribution. The methodology is applied here for the case of rainfed wheat and grain maize across Europe using an ensemble of crop models under three climate change scenarios with simulations conducted at 25 km resolution. Under climate change, maize generally displayed shorter return periods of yield failures (with changes under RCP 4.5 between -0.3 and 0 years compared to the baseline scenario) associated with a shift of the yield distribution towards lower values and changes in shape of the distribution that further reduced the frequency of high yields. This response was prominent in the areas characterized in the baseline scenario by high yields and relatively long return periods of failure. Conversely, for wheat, yield failures were projected to become less frequent under future scenarios (with changes in the return period of -0.1 to +0.4 years under RCP 4.5) and were associated with a shift of the distribution towards higher values and a change in shape increasing the frequency of extreme yields at both ends. Our study offers an approach to quantify the changes in yield distributions that drive crop yield failures. Actual risk assessments additionally require models that capture the variety of drivers determining crop yield variability and scenario climate input data that samples the range of probable climate variation.

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