Volume- 9
Issue- 1
Year- 2022
DOI: 10.55524/ijirem.2022.9.1.49 | DOI URL: https://doi.org/10.55524/ijirem.2022.9.1.49
This is an Open Access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0) (http://creativecommons.org/licenses/by/4.0)
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Dr. Anubhav Soni , Pooran Singh
Dry spells ranging from years to decades have happened many times throughout history. North America, West Africa, and East Asia, for example, have seen significant changes in the past century. Asia. Droughts were most likely caused by unusual tropical sea surface temperatures. Temperatures (SSTs), with La Nina-like SST anomalies causing dryness in parts of the country. Drought in East China is being caused by El Nino-like SSTs in North America. Across Africa, warming in the Atlantic and a southern shift of the hottest SSTs Droughts in the Sahel have been blamed on the Indian Ocean. Local feedbacks may be useful. Intensify and extend the drought Since the 1970s, global aridity has risen dramatically. Due to recent dryness in Africa, southern Europe, and East and South Asia in the 1970s, as well as eastern Australia. Despite the El Nino-Southern Oscillation (ENSO), tropical cyclones continue to exist. Atlantic SSTs and Asian monsoons have aided the current dryness. The demand for moisture in the atmosphere has risen because of recent warming, and this has likely changed the landscape. Both of these factors contribute to the drying of the atmosphere. Models of climate change. In the twenty-first century, much of Africa and southern Europe saw increasing aridity and the Middle East, as well as the majority of North and South America, Australia, and Southeast Asia Region.
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Assistant Professor, Department of Management, Sanskriti University, Mathura, Uttar Pradesh
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