Applied Climate

Drought characteristics and regression models of drought characteristics and response factors of various climatic areas in Inner Mongolia during main crop growing season

Expand
  • 1. Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Hohhot 010018, Inner Mongolia, China
    2. Institute of Water Resources for Pastoral Area, China Institute of Water Resources and Hydropower Research, Hohhot 010020, Inner Mongolia, China

Received date: 2022-04-11

  Revised date: 2022-06-27

  Online published: 2022-10-25

Abstract

With the foundation of global climate change in recent years, droughts in various climatic areas in Inner Mongolia may bring unpredictable disaster risks to local agricultural production. The whole region was divided into five climatic areas, and monthly data was received from 46 meteorological stations from 1981 to 2012. Twenty meteorological stations from 2014 to 2020 were selected to calculate the different time scales of the standardized precipitation evapotranspiration index (SPEI) using precipitation and reference evapotranspiration from the Penman-Monteith method to reveal the drought characteristics and its dominant meteorological factors during the crop growing season (May-September) in Inner Mongolia. A monthly drought during the crop growing season was revealed. The high-incidence month and region of drought in the growing season in various climatic areas were identified by the SPEI of a 1-month scale, and a stepwise linear regression method was selected and verified to extract the dominant meteorological factors driving the drought in each month and the whole growing season in various climatic areas. Results indicated that the following: (1) from the interannual changes, the drought from 1998 to 2008 was more serious, and the drought in other years was less serious. (2) The largest drought area and degree appeared in May during the crop growing season. The probability of moderate drought in the moist and semi-humid area was 37% higher compared to the hyper-arid area, while the extreme drought probably occurred in the moist and semi-humid area and dry and semi-humid area. (3) Dominant meteorological factors driving the drought varied in the crop growth period of various climatic areas in Inner Mongolia. Precipitation and a minimum temperature were the main impact factors for a drought in the crop growing season. (4) Using limited meteorological data, the regression models in each climate region performance well can be used to estimate the monthly SPEI. The results provide a theoretical basis for scientific evaluation of drought characteristics in the spring maize growing season and formulates reasonable measures of response to the drought.

Cite this article

GAO Xiaoyu,TANG Pengcheng,ZHANG Sha,QU Zhongyi,YANG Wei . Drought characteristics and regression models of drought characteristics and response factors of various climatic areas in Inner Mongolia during main crop growing season[J]. Arid Zone Research, 2022 , 39(5) : 1410 -1427 . DOI: 10.13866/j.azr.2022.05.07

References

[1] Dai A, Trenberth K E, Qian T. A global dataset of Palmer Drought Severity index for 1870-2002: Relationship with soil moisture and effects of surface warming[J]. Journal of Hydrometeorology, 2004, 5(6): 1117-1130.
[2] 郑大玮, 李茂松, 霍治国. 农业灾害与减灾对策[M]. 北京: 中国农业大学出版社, 2013.
[2] [Zheng Dawei, Li Maosong, Huo Zhiguo. Agricultural Disasters and Countermeasures for Disaster Reduction[M]. Beijing: China Agricultural University Press, 2013. ]
[3] 马柱国, 符淙斌. 1951—2004 年中国北方干旱化的基本事实[J]. 科学通报, 2006, 51(20): 2429-2439.
[3] [Ma Zhuguo, Fu Congbin. Characteristics of aridification over northern China during 1951-2004[J]. Chinese Science Bulletin, 2006, 51(20): 2429-2439. ]
[4] 王娜, 王靖, 冯利平, 等. 华北平原冬小麦-夏玉米轮作区采用“两晚”技术的产量效应模拟分析[J]. 中国农业气象, 2015, 36(5): 611-618.
[4] [Wang Na, Wang Jing, Feng Liping, et al. Modeling the impact of “Double-Delay” technology on yield of wheat-maize cropping system in the North China Plain[J]. Chinese Journal of Agrometeorology, 2015, 36(5): 611-618. ]
[5] 周扬, 李宁, 吉中会, 等. 基于SPI 指数的1981—2010年内蒙古地区干旱时空分布特征[J]. 自然资源学报, 2013, 28(10): 1694-1706.
[5] [Zhou Yang, Li Ning, Ji Zhonghui, et al. Temporal and spatial patterns of droughts based on standard precipitation index(SPI) in Inner Mongolia during 1981-2010[J]. Journal of Natural Resource, 2013, 28(10): 1694-1706. ]
[6] 刘荣花, 朱自玺, 方文松, 等. 华北平原冬小麦干旱灾损风险区划[J]. 生态学杂志, 2006, 25(9): 1068-1072.
[6] [Liu Ronghua, Zhu Zixi, Fang Wensong, et al. Risk regionalization of yield loss caused by drought for winter wheat in North China Plain[J]. Chinese Journal of Ecology, 2006, 25(9): 1068-1072. ]
[7] Palmer W C. Meteorology Drought[R]. Washington: No.30 US Department of Commerce, Weather Bureau Washington, 1965.
[8] 周丹, 张勃, 罗静, 等. 基于SPEI 的华北地区近50 年干旱发生强度的特征及成因分析[J]. 自然灾害学报, 2014, 23(4): 192-202.
[8] [Zhou Dan, Zhang Bo, Luo Jing, et al. SPEI-based intensity characteristics and cause analysis of drought in North China during recent 50 years[J]. Journal of Natural Disasters, 2014, 23(4): 192-202. ]
[9] Hayes M J, Svoboda M D, Wilhite D A, et al. Monitoring the 1996 drought using the standardized precipitation index[J]. Bulletin of the American Meteorological Society, 1999, 80(3): 429-438.
[10] 周磊, 武建军, 吕爱峰, 等. 华北不同地表覆盖类型区干旱演变特征[J]. 地理研究, 2012, 31(4): 597-607.
[10] [Zhou Lei, Wu Jianjun, Lv Aifeng, et al. Drought evolution of different land cover regions in North China[J]. Geographical Research, 2012, 31(4): 597-607. ]
[11] 吴英杰, 李玮, 王文君, 等. 基于降水量距平百分率的内蒙古地区干旱特征[J]. 干旱区研究, 2019, 36(4): 943-952.
[11] [Wu Yingjie, Li Wei, Wang Wenjun, et al. Drought characteristics in Inner Mongolia based on precipitation anomaly percentage[J]. Arid Zone Research, 2019, 36(4): 943-952. ]
[12] 朱烨, 靳鑫桐, 刘懿, 等. 基于短时间尺度自适应帕尔默干旱指数的中国干旱演变特征分析[J]. 水资源保护, 2022, 38(4): 124-130.
[12] [Zhu Ye, Jin Xintong, Liu Yi, et al. Drought characteristics analysis in China based on self-calibrating Palmer drought severity index in a short time scale[J]. Water Resources Protection, 2022, 38(4): 124-130. ]
[13] 王林, 陈文. 标准化降水蒸散指数在中国干旱监测的适用性分析[J]. 高原气象, 2014, 33(2): 423-431.
[13] [Wang Lin, Chen Wen. Applicability analysis of standardized precipitation evapotranspiration index in drought monitoring in China[J]. Plateau Meteorology, 2014, 33(2): 423-431. ]
[14] Vicente-Serrano S M, Begueria S, Lopez-Moreno J I. A multiscalar drought index sensitive to global warming: The standardized precipitation evapotranspiration index[J]. Journal of Climate, 2010, 23(7): 1696-1718.
[15] 刘珂, 姜大膀. 基于两种潜在蒸散发算法的SPEI对中国干湿变化的分析[J]. 大气科学, 2015, 39(1): 23-36.
[15] [Liu Ke, Jiang Dabang. Analysis of dryness/wetness over China using standardized precipitation evapotranspiration index based on two evapotranspiration algorithms[J]. Chinese Journal of Atmospheric Sciences, 2015, 39(1): 23-36. ]
[16] 庄少伟, 左洪超, 任鹏程, 等. 标准化降水蒸发指数在中国区域的应用[J]. 气候与环境研究, 2013, 18(5): 617-625.
[16] [Zhuang Shaowei, Zuo Hongchao, Ren Pengcheng, et al. Application of standardized precipitation evapotranspiration index in China[J]. Climatic and Environmental Research, 2013, 18(5): 617-625. ]
[17] 刘宇, 李雯晴, 刘招, 等. 基于SPEI渭北黄土台塬区干旱时空演变特征[J]. 水土保持研究, 2021, 28(1): 109-117.
[17] [Liu Yu, Li Wenqing, Liu Zhao, et al. Spatial and temporal evolution characteristics of the drought in Weibei loess tableland area based on SPEI[J]. Research of Soil and Water Conservation, 2021, 28(1): 109-117. ]
[18] 张煦庭, 潘学标, 徐琳, 等. 基于降水蒸发指数的1960—2015年内蒙古干旱时空特征[J]. 农业工程学报, 2017, 33(15): 190-199.
[18] [Zhang Xuting, Pan Xuebiao, Xu Lin, et al. Analysis of spatio-temporal distribution of drought characteristics based on SPEI in Inner Mongolia during 1960-2015[J]. Transactions of the Chinese Society of Agricultural Engineering, 2017, 33(15): 190-199. ]
[19] 任晓东. 内蒙古不同气候区ET0估算方法(FAO-PM温度法和Hargreaves-Samani法)的适用性评价[D]. 呼和浩特: 内蒙古农业大学, 2014.
[19] [Ren Xiaodong. Assessment of ET0 Estimation Methods (FAO-PM Temperature and Hargreaves-Samani Methods) in Different Climates of Inner Mongolia[D]. Hohhot: Inner Mongolia Agricultural University, 2014. ]
[20] 王潇潇, 潘学标, 顾生浩, 等. 内蒙古地区参考作物蒸散变化特征及其气象影响因子[J]. 农业工程学报, 2015, 31(增刊1): 142-152.
[20] [Wang Xiaoxiao, Pan Xuebiao, Gu Shenghao, et al. Trend in reference crop evapotranspiration and meteorological factors affecting trends in Inner Mongolia[J]. Transactions of the Chinese Society of Agricultural Engineering, 2015, 31(Suppl.1): 142-152. ]
[21] Allen R G, Pereira L S, Raes D, et al. Crop Evapotranspiration Guidelines for Computing Crop Water Requirements[M]. Roma Italy: FAO Irrigation and Drainage, 1998: 56.
[22] 李伟光, 易雪, 侯美亭, 等. 基于标准化降水蒸散指数的中国干旱趋势研究[J]. 中国生态农业学报, 2012, 20(5): 643-649.
[22] [Li Weiguang, Yi Xue, Hou Meiting, et al. Standardized precipitation evapotranspiration index shows drought trends in China[J]. Chinese Journal of Eco-Agriculture, 2012, 20(5): 643-649. ]
[23] 李崇瑞, 游松财, 武永峰. 东北地区干旱特征与春玉米生长季干旱主导气象因子[J]. 农业工程学报, 2020, 36(19): 97-106.
[23] [Li Chongrui, You Songcai, Wu Yongfeng. Drought characteristics and dominant meteorological factors driving drought in spring maize growing season in Northeast China[J]. Transactions of the Chinese Society of Agricultural Engineering, 2020, 36(19): 97-106. ]
[24] Liu S, Kang W, Wang T. Drought variability in Inner Mongolia of northern China during 1960-2013 based on standardized precipitation evapotranspiration index[J]. Environmental Earth Sciences, 2016, 75(2): 1-14.
[25] Huang J, Sun S L, Xue Y, et al. Changing characteristics of precipitation during 1960-2012 in Inner Mongolia, northern China[J]. Meteorology and Atmospheric Physics, 2015, 127(3): 257-271.
[26] 那音太. 基于SPI 指数的近50 a内蒙古地区干旱特征分析[J]. 干旱区资源与环境, 2015, 29(5): 161-166.
[26] [Na Yintai. Drought characteristics in Inner Mongolia based on the SPI index in the last 50 years[J]. Journal of Arid Land Resources and Environment, 2015, 29(5): 161-166. ]
[27] 李秋月, 潘学标, 王丽, 等. 内蒙古地区气候资源变化趋势分析[J]. 中国农业气象, 2011, 32(增刊): 19-23.
[27] [Li Qiuyue, Pan Xuebiao, Wang Li, et al. Analysis of the trend of climate resources change in Inner Mongolia[J]. Chinese Journal of Agrometeorology, 2011, 32(Suppl.): 19-23. ]
Outlines

/