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How extremes in surface incident solar radiation shape its long-term trends in China and Europe

Datos Bibliográficos

ID15550486
AutoresYanyi He (0000-0002-6326-0550, Sun Yat-sen University, autor de correspondencia), K Yang (0000-0002-0809-2371, Ocean Renewable Power Company (United States)), Mingyu Zhang (0000-0003-3628-0983, Sun Yat-sen University), Jingjing Zhou (0000-0003-4594-7743, Sun Yat-sen University), Chenlu Li (0000-0002-4561-970X, Xi'an University of Architecture and Technology), Xin Zhang (0000-0003-0184-5868), Xin mei Zhang (Beijing Hospital), Xiaoyue Tan (0000-0001-9989-0573, Hong Kong Polytechnic University), Kaicun Wang (0000-0002-7414-5400, Peking University)
Año2026
Volumen21
Número3
Páginas034030-034030
Fecha de publicación2026-02-03
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaEnvironmental Research Letters (JOURNAL)
Identificadores de la revistaISSN: 1748-9326 • E-ISSN: 1748-9326
EditorialIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/ae4112
OpenAlexW7127326965
IdiomaEN
Referencias citadas41

Although extremes of surface incident solar radiation ( R s ) are critical for climate and energy assessments, their long-term variations and contributions to R s trends remain poorly understood. Leveraging the recently homogenized daily R s data at ∼2600 stations across China and Europe during 1961–2022, this study provided the first quantification of long-term variations in extremely low ( R s 10p) and high ( R s 90p) R s and their contributions to R s trends. During the dimming period, increasing R s 10p and decreasing R s 90p frequencies, along with increased magnitudes, jointly led to the dimming over China and Europe. Europe began to steadily brighten after 1980, due to early air pollution emission controls and reduced cloud cover, which reversed the frequency trends of R s 10p and R s 90p and intensified the severities of both extremes. In contrast, dimming in China persisted until 2014, only transitioning to brightening after the implementation of stricter emission controls which increased R s 90p frequencies but attenuated the severities of both extremes. Overall, R s extremes jointly regulated R s trends: China’s brightening was positively contributed by both extremes, while Europe’s brightening was dominated by R s 90p but partially offset by R s 10p. These findings underscore the pivotal role of extremes in shaping overall R s trends and highlight their importance for accurately assessing regional solar energy availability under global climate change

China · Climate change · Global warming · Offset (computer science · Surface air temperature · Atmospheric aerosols and clouds · Climate Change and Geoengineering · Solar Radiation and Photovoltaics · Radiation

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