Abstract

The dry-hot wind climate is one of the major agro-meteorological disasters associated with high temperature, low humidity, and specific wind forces, which seriously affects the yield of wheat in the North China Plain. A field experiment was conducted to investigate the field microclimate, net photosynthetic rate, chlorophyll content of flag leaves, grain filling rate, and wheat yield after sprinkler misting under the condition of a dry-hot wind climate in the 2018 and 2019 seasons. Two travel speeds, full and half speed, and the corresponding irrigation amounts of 2.5 and 5 mm were used by a center pivot irrigation system during dry-hot wind conditions. A treatment without irrigation was applied as a control. The results showed that the air temperature and relative air humidity were greatly improved within 60 min after irrigation, especially in the upper part of the canopy. The net photosynthetic rate of flag leaves under 5 mm irrigation was higher than that under 2.5 mm irrigation during the middle and late grain filling periods. The adverse effects of dry-hot wind on the chlorophyll content of the flag leaves were mainly concentrated in the late grain filling stage. In the two years of the experiment, the average 1000-grain weights of 5 and 2.5 mm of irrigation treatments were 4.3 and 2.8% higher, and the grain yields were 5.8 and 3.3% higher, respectively, than those of the non-irrigated yields. Overall, applying a small amount of water between 12:00–14:00 with a center pivot before the occurrence of dry-hot wind is an effective means to regulate the field microclimate and produce more yield in the North China Plain.

Highlights

  • IntroductionGlobal warming is causing an increasing amount of extreme weather and climate events, which seriously affects agroecosystems and causes increased instability in agricultural production [1]

  • Dry-hot wind events are characterized by maximum day temperatures greater than 30 ◦ C, relative humidity less than 30%, and a wind speed greater than 3 m s−1 at approximately 14:00 local time in the North China Plain [3,4]

  • In 2019, a significant (p < 0.05) difference in SPAD among the three treatments occurred after 4 June (Figure 7). These results showed that the adverse effects of dry-hot wind on chlorophyll content in the flag leaves were mainly concentrated in the late filling stage

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Summary

Introduction

Global warming is causing an increasing amount of extreme weather and climate events, which seriously affects agroecosystems and causes increased instability in agricultural production [1]. The frequency of dry-hot wind occurrence has been increasing recently in China due to climate warming [2]. Dry-hot wind events are characterized by maximum day temperatures greater than 30 ◦ C, relative humidity less than 30%, and a wind speed greater than 3 m s−1 at approximately 14:00 local time in the North China Plain [3,4]. The most concentrated period of dry-hot wind is from mid and late May to early June in the North China Plain, during which winter wheat (Triticum aestivum L.) is in the anthesis and filling stage [5].

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