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Analysis of Climate Variability and Its Implications on Rangelands in the Limpopo Province.
- Source :
- Climate (2225-1154); Jan2024, Vol. 12 Issue 1, p2, 27p
- Publication Year :
- 2024
-
Abstract
- In recent decades, southern Africa has experienced a shift towards hotter and drier climate conditions, affecting vital sectors like agriculture, health, water, and energy. Scientific research has shown that the combination of high temperatures and unreliable rainfall can have detrimental effects on agricultural production. Thus, this study focused on assessing climate variability, with implications on rangelands in the Limpopo Province of South Africa over 38 years. Historical climate data from 15 stations, including rainfall and minimum and maximum temperatures from 1980 to 2018, were analysed. To achieve the main objective, various statistics including mean, standard deviation, and coefficient of variation (CV) were computed for all variables across four seasons. The results highlighted significant variability in rainfall, with Musina (71.2%) and Tshiombo (88.3%) stations displaying the highest variability during the September-to-April season. Both minimum and maximum temperatures displayed low variability. The Mann–Kendall test revealed both increasing and decreasing trends in minimum temperatures and rainfall across different stations. Notably, there was a significant increase in maximum temperatures. This study provides valuable climate information for decision makers, aiding in the planning and management of agricultural activities, particularly in understanding how climate variations affect forage availability in rangelands. [ABSTRACT FROM AUTHOR]
- Subjects :
- RANGELANDS
RAINFALL
LOW temperatures
CLIMATE change
FARM management
HIGH temperatures
Subjects
Details
- Language :
- English
- ISSN :
- 22251154
- Volume :
- 12
- Issue :
- 1
- Database :
- Complementary Index
- Journal :
- Climate (2225-1154)
- Publication Type :
- Academic Journal
- Accession number :
- 175050272
- Full Text :
- https://doi.org/10.3390/cli12010002