Potential impact of future climate change on sugarcane under dryland conditions in Mexico

被引:15
作者
Baez-Gonzalez, A. D. [1 ]
Kiniry, J. R. [2 ]
Meki, M. N. [3 ]
Williams, J. R. [3 ]
Alvarez Cilva, M. [4 ]
Ramos Gonzalez, J. L. [1 ]
Magallanes Estala, A. [5 ]
机构
[1] INIFAP, Campo Expt Pabellon, Pabellon De Arteaga, Aguascalientes, Mexico
[2] ARS, Grassland Soil & Water Res Lab, USDA, Temple, TX USA
[3] Blackland Res & Extens Ctr, AgriLife Res, Temple, TX USA
[4] INIFAP, Campo Expt Tecoman, Tecoman, Colima, Mexico
[5] INIFAP, Campo Expt Rio Bravo, Rio Bravo, Tamaulipas, Mexico
关键词
ALMANAC model; CP; 72-2086; Mexican sugarcane; midsummer drought; sugarcane flowering; 1ST REPORT; MODEL; MAIZE; EVAPOTRANSPIRATION; ALMANAC; AFRICA; GROWTH; YIELD; PLANT; CO2;
D O I
10.1111/jac.12278
中图分类号
S3 [农学(农艺学)];
学科分类号
090104 [作物信息科学与技术];
摘要
Assessments of impacts of future climate change on widely grown sugarcane varieties can guide decision-making and help ensure the economic stability of numerous rural households. This study assessed the potential impact of future climatic change on sugarcane grown under dryland conditions in Mexico and identified key climate factors influencing yield. The Agricultural Land Management Alternatives with Numerical Assessment Criteria (ALMANAC) model was used to simulate sugarcane growth and yield under current and future climate conditions. Management, soil and climate data from farm sites in Jalisco (Pacific Mexico) and San Luis Potosi (Northeastern Mexico) were used to simulate baseline yields. Baseline climate was developed with 30-year historical data from weather stations close to the sites. Future climate for three decadal periods (2021-2050) was constructed by adding forecasted climate values from downscaled outputs of global circulation models to baseline values. Climate change impacts were assessed by comparing baseline yields with those in future decades under the A2 scenario. Results indicate positive impacts of future climate change on sugarcane yields in the two regions, with increases of 1%-13% (0.6-8.0Mg/ha). As seen in the multiple correlation analysis, evapotranspiration explains 77% of the future sugarcane yield in the Pacific Region, while evapotranspiration and number of water and temperature stress days account for 97% of the future yield in the Northeastern Region. The midsummer drought (canicula) in the Pacific Region is expected to be more intense and will reduce above-ground biomass by 5%-13% (0.5-1.7Mg/ha) in July-August. Harvest may be advanced by 1-2months in the two regions to achieve increases in yield and avoid early flowering that could cause sucrose loss of 0.49Mgha(-1)month(-1). Integrating the simulation of pest and diseases under climate change in crop modelling may help fine-tune yield forecasting.
引用
收藏
页码:515 / 528
页数:14
相关论文
共 66 条
[1]
Aguilar N., 2004, MEXICO CANA AZUCAR, V22, P19
[2]
Allen L. H. Jr., 2011, Current Topics in Plant Biology, Volume 12, P171
[3]
Allen R. G., 1998, FAO Irrigation and Drainage Paper
[4]
[Anonymous], 1988, SOIL MAP WORLD
[5]
[Anonymous], 2014, DIAR OF FED PROGR NA, P3
[6]
Historical Warnings of Future Food Insecurity with Unprecedented Seasonal Heat [J].
Battisti, David. S. ;
Naylor, Rosamond L. .
SCIENCE, 2009, 323 (5911) :240-244
[7]
Spatial forecasting of switchgrass productivity under current and future climate change scenarios [J].
Behrman, Kathrine D. ;
Kiniry, James R. ;
Winchell, Michael ;
Juenger, Thomas E. ;
Keitt, Timothy H. .
ECOLOGICAL APPLICATIONS, 2013, 23 (01) :73-85
[8]
Sensitivity analysis of 18 different potential evapotranspiration models to observed climatic change at German climate stations [J].
Bormann, Helge .
CLIMATIC CHANGE, 2011, 104 (3-4) :729-753
[9]
Yield-Gap Analysis of a Homogeneous Area and Zonification of a Sugarcane Mill Region in Oaxaca, Mexico [J].
Bravo-Mosqueda, Ernesto ;
Delia Baez-Gonzalez, Alma ;
Alberto Tinoco-Alfaro, Carlos ;
Mariles-Flores, Veronica ;
Osuna-Ceja, Esteban .
JOURNAL OF CROP IMPROVEMENT, 2014, 28 (06) :772-794
[10]
Evaporation and potential evapotranspiration in India under conditions of recent and future climate change [J].
Chattopadhyay, N ;
Hulme, M .
AGRICULTURAL AND FOREST METEOROLOGY, 1997, 87 (01) :55-73