尽管气候趋势温和,但非洲南部的作物生产率停滞不前
David B Lobell1,2, Richard J Lee3,4
1Department of Earth System Science, Stanford University, Stanford, CA, USA. dlobell@stanford.edu.
Nature food
|July 15, 2025
概括
南非 非洲南部 非洲南部
科学领域:
- 农业科学 农业科学
- 气候科学是气候科学.
- 食品安全研究 食品安全研究
背景情况:
- 南非经历了严重的粮食不安全.
- 预计的农业气候下降威胁到该地区的农业产量.
- 官方作物统计数据可能不准确地反映地面现实.
研究的目的:
- 分析过去20年南非农田生产率趋势.
- 为了将卫星产生的生产率数据与官方作物统计数据进行比较.
- 调查气候趋势在观测到的生产率变化中的作用.
主要方法:
- 利用多个卫星测量来评估耕地生产力.
- 分析了区域气候趋势,包括降雨量和温度.
- 将卫星数据与南部非洲的官方作物统计数据进行比较.
主要成果:
- 南非大部分地区的耕地生产率停滞不前.
- 与该地区其他地区相比,南非的生产率趋势不同.
- 观察到的气候趋势 (降雨量增加,变暖减少) 并不能解释生产率停滞.
结论:
- 卫星数据显示,生产率停滞不前,与官方报告不符.
- 目前的气候趋势无法解释所观察到的农业停滞.
- 迫切的战略变革是必要的,在气候影响恶化之前,解决粮食不安全问题.
相关概念视频
What is Climate?
18.9K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
18.9K
The Calvin Benson Cycle
4.7K
Ribulose 1,5- bisphosphate carboxylase/oxygenase (RuBisCo) is a critical enzyme that catalyzes carbon dioxide assimilation during photosynthesis. However, it is an inefficient enzyme, having an extremely slow catalytic rate. A typical enzyme can process about a thousand molecules per second; however, RuBisCo fixes only around three-carbon dioxides per second. Photosynthetic cells compensate for this slow rate by synthesizing very high amounts of RuBisCo, making it the most abundant single...
4.7K
Adaptations that Reduce Water Loss
26.3K
Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
26.3K
Global Climate Change
24.8K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.8K
Primary Production
24.0K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
24.0K
Responses to Heat and Cold Stress
13.9K
Every organism has an optimum temperature range within which healthy growth and physiological functioning can occur. At the ends of this range, there will be a minimum and maximum temperature that interrupt biological processes.
13.9K


