WebMay 26, 2024 · Woo et al. ( 2024 ), using a high-resolution (40 km) atmospheric general circulation model, projected an increase in summer precipitation over the Indian subcontinent of 7–10% under the RCP4.5 scenario and 14–18% under RCP8.5 for the mid to the end of the twenty-first century. WebThere is even an East Asian monsoon that brings summer rain to China, Japan, and Korea, but it is caused by a different type of wind pattern that is associated with the jet stream. Monsoons bring large amounts of rain to a location, often leading to large-scale vegetation growth. University of Oregon The Americas
Projections of Precipitation and Temperature over the South …
WebJun 14, 2024 · A record-breaking Meiyu-Baiu rainfall hit East Asia in June–July 2024. The warm Indian Ocean (IO) has been identified as a primary cause, but it cannot explain the heavy rainfall in July, a striking characteristic of the 2024 Meiyu-Baiu rainfall. WebJun 18, 2015 · The modern Asian summer monsoon limit is shown by a green dashed line. Areas above 3000 m (above sea level) are shaded in grey. The Chinese Loess Plateau is shaded in light yellow. Daihai, Qinghai ... Metrics - East Asian summer monsoon precipitation variability since the last ... danish names last names
Impact of the Upper Tropospheric Cooling Trend over Central Asia …
WebApr 10, 2024 · The East Asian summer monsoon (EASM) is a unique regional monsoon in the extratropics involving not only tropical but midlatitude processes. Most of the previous studies identified the role of condensational heating which is largely relevant to the tropical moisture transport in determining the dynamical structure of EASM. WebJul 30, 2024 · Lu et al. (2024) pointed out that the trend of the Holocene EASM rainfall in southern China (28°–38°N, 112°–124°E) matched with the decreasing trend in the Northern hemisphere solar insolation (NHSI), while the maximum rainfall in arid/semi-arid northern China (38°–53°N, 80°–105°E) lags behind the peak insolation by ∼4–5 ka. WebJan 23, 2024 · With the weakening of EASM circulation, the spatial distribution changes of summer precipitation in eastern China occurred in the mid and late 1970s. Precipitation increased in the middle and lower reaches of the Yangtze River, while precipitation in northern China and southern China decreased. birthday cards delivered to recipient