4.7 Article

Rainfall Variability and Trends over the African Continent Using TAMSAT Data (1983-2020): Towards Climate Change Resilience and Adaptation

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REMOTE SENSING
卷 14, 期 1, 页码 -

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MDPI
DOI: 10.3390/rs14010096

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rainfall variability; rainfall trend; TAMSAT data; climate change; climate hazard; Africa

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This study examines rainfall variability and trends in Africa using TAMSAT data from 1983 to 2020. The findings show that certain regions have higher annual rainfall trends, while others have lower trends. There is a statistically significant increase in rainfall in countries located in the northern and central parts of Africa, while no significant change is observed in countries in the southern and eastern regions. The study also reveals a significant increase in rainfall in certain tropical climate zones. These findings are crucial for decision-makers involved in crop planning and water resource management.
This study reveals rainfall variability and trends in the African continent using TAMSAT data from 1983 to 2020. In the study, a Mann-Kendall (MK) test and Sen's slope estimator were used to analyze rainfall trends and their magnitude, respectively, under monthly, seasonal, and annual timeframes as an indication of climate change using different natural and geographical contexts (i.e., sub-regions, climate zones, major river basins, and countries). The study finds that the highest annual rainfall trends were recorded in Rwanda (11.97 mm/year), the Gulf of Guinea (river basin 8.71 mm/year), the tropical rainforest climate zone (8.21 mm/year), and the Central African region (6.84 mm/year), while Mozambique (-0.437 mm/year), the subtropical northern desert (0.80 mm/year), the west coast river basin of South Africa (-0.360 mm/year), and the Northern Africa region (1.07 mm/year) show the lowest annual rainfall trends. There is a statistically significant increase in the rainfall in the countries of Africa's northern and central regions, while there is no statistically significant change in the countries of the southern and eastern regions. In terms of climate zones, in the tropical northern desert climates, tropical northern peninsulas, and tropical grasslands, there is a significant increase in rainfall over the entire timeframe of the month, season, and year. This implies that increased rainfall will have a positive effect on the food security of the countries in those climatic zones. Since a large percentage of Africa's agriculture is based only on rainfall (i.e., rain-fed agriculture), increasing trends in rainfall can assist climate resilience and adaptation, while declining rainfall trends can badly affect it. This information can be crucial for decision-makers concerned with effective crop planning and water resource management. The rainfall variability and trend analysis of this study provide important information to decision-makers that need to effectively mitigate drought and flood risk.

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