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A Bio-Economic Crop Yield Response (BECYR) Model for Corn and Soybeans in Ontario, Canada for 1959-2013

Climate change is a widely discussed topic, and its effect on crop production has drawn attention. The projected reduction in crop yields due to the changing climate in some regions has raised concern. Several studies have estimated the effects of changing climate on crop yields. These models include variables reflecting the effects of weather, technology and land quality. Many models, however, have not included prices, groundwater level, or CO2 concentration. In Table 1, we compared the variables included those previous econometric crop yield modelling research for corn and soybeans with the variables included in our study.

Xu Q, Fox G, McKenney DW, Parkin G, Li Z.

Sci Rep. 2020 Apr 24;10(1):7006. doi: 10.1038/s41598-020-63765-3.

Abstract

Climate change is a widely discussed topic, and its effect on crop production has drawn attention. The projected reduction in crop yields due to the changing climate in some regions has raised concern. Several studies have estimated the effects of changing climate on crop yields. These models include variables reflecting the effects of weather, technology and land quality. Many models, however, have not included prices, groundwater level, or CO2 concentration. In Table 1, we compared the variables included those previous econometric crop yield modelling research for corn and soybeans with the variables included in our study. This paper presents estimates of the effects of changing climate on crop yields for grain corn and soybeans in Ontario, Canada, for 1959-2013. We were able to use a database that is more comprehensive with respect to explanatory variables than some previous efforts had available. Our model includes climate variables, prices, land quality, groundwater level, CO2 concentration, and a time trend. Our results indicate that trends in temperature and precipitation during our study period have not yet resulted in appreciable threats to crop yields in the region.

 

See https://www.ncbi.nlm.nih.gov/pubmed/32332869

 

Figure 1: Actual and Proxy of Monthly CO2 Concentration (ppm) in Hawaii and Ontario for 1959–2016. Black line: the actual CO2 data in Mauna, Hawaii (1959–2016) from National Oceanic and Atmospheric Administration. Blue line: the actual CO2 data in Egbert, Ontario (2005–2016) from The World Data Center for Greenhouse Gases. Redline: the proxy of CO2 data in Egbert, Ontario (1959–2004). Discontinuities are due to missing values. The actual Hawaii and Ontario CO2 data show a similar increasing trend, but the CO2 concentration in Ontario varies more than in Hawaii. In addition, the CO2 level in Ontario reaches a peak between November and April and drops from May till July/August. The CO2 concentration in Hawaii peaks in May and drops from June to October. Variation in the CO2 concentration in Ontario reflect the reduction in photosynthesis during the winter months. Photosynthesis is less variable during the year in Hawaii. So, we regressed the monthly Ontario CO2 concentration on the linear corresponding value for Hawaii from 2005 to 2016. We then used the estimated coefficients from the regression to calculate the proxy serving for Ontario for 1959–2004, by substituting the Hawaii observations into the regression equation. See Table S6 for the estimated results and Fig. S2 for the residual plot in the CO2 regression model.

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