The Indian summer monsoon keeps the Arabian Peninsula hot and dry
Modeling shows that the Indian Summer Monsoon can trigger heatwaves and sandstorms on the Arabian Peninsula
The influence of the Indian summer monsoon on the climate of the Arabian Peninsula has been described for the first time by KAUST researchers. This could lead to more accurate models for forecasting how the monsoons impact the region’s weather.
The Arabian Peninsula is one of the world’s most arid and water-stressed regions, with the summer months characterized by frequent heat waves and dust storms. Various large-scale processes, such as the El Niño Southern Oscillation and the North Atlantic Oscillation, play a significant role on the region’s weather and climate.
Heat generated by the Indian summer monsoon rains also influences the Arabian Peninsula summer monsoon circulation, affecting the regional climate through a variety of interconnected physical processes.
However, the role played by the Indian summer monsoon in modulating the Arabian Peninsula’s climate is little understood, particularly the way in which the region’s climate variability is affected by year-to-year variations, classified as strong and weak Indian summer monsoon years.
Now, Raju Attada, and a team lead by Ibrahim Hoteit, in collaboration with researchers from the Indian Institute of Tropical Meteorology, have investigated how annual variations in the Indian Summer Monsoon impact the Arabian Peninsula’s climate and the changes associated with strong and weak monsoons.
“The Arabian Peninsula is a water-scarce region and one of the most vulnerable in the world,” says Attada. “Therefore, understanding how changes in Indian summer monsoon activity influence the Arabian Peninsula summer climate is of great importance as it impacts almost every aspect of life, from weather extremes, pollution and health to water resources and renewable energy.”
To model the influence of the Indian summer monsoon, the team used datasets from the European Centre for Medium Range Weather Forecasts’ twentieth-century reanalysis (ERA-20C) for the period 1901–2010. This contains data on the physical processes, such as horizontal and vertical wind speeds, air temperatures and humidity levels, that influence the region’s climate.
The researchers found that air circulation systems, or jet streams, control many aspects of the Arabian Peninsula climate and are themselves greatly influenced by the Indian summer monsoon. Moreover, circulation in the region is dominated by subsidence of monsoon circulation, in which atmospheric waves in high altitudes triggered by the Indian summer monsoon propagate westward and sink from the upper to the lower atmosphere, increasing the aridity of the region.
“Our work shows that these jet streams can trigger severe heat waves and sandstorms, and that their influence is greatest during strong monsoons,” explains Attada. “Pollutants and dust transported from eastern European industrial zones and the Sahara desert can also reduce the region’s air quality.”
This article was first published by Springer Nature. Read the original article here.