2009
DOI: 10.1007/s00704-009-0213-y
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Solar dimming and its impact on estimating solar radiation from diurnal temperature range in China, 1961–2007

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Cited by 37 publications
(42 citation statements)
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“…Decreased NRD in the winter thus seems to be consistent with increased SSD in the LH and HHM during the same season (Table 4). A change in SR could alter the diurnal temperature range by influencing maximum temperatures (Padma Kumari et al, 2007;Ye et al, 2009). The increasing trend in maximum temperatures during the winter season in the Himalayan regions (Shrestha et al, 1999) is therefore consistent with the increasing trends of SSD in the HHM regions in the present study.…”
Section: Discussionsupporting
confidence: 76%
“…Decreased NRD in the winter thus seems to be consistent with increased SSD in the LH and HHM during the same season (Table 4). A change in SR could alter the diurnal temperature range by influencing maximum temperatures (Padma Kumari et al, 2007;Ye et al, 2009). The increasing trend in maximum temperatures during the winter season in the Himalayan regions (Shrestha et al, 1999) is therefore consistent with the increasing trends of SSD in the HHM regions in the present study.…”
Section: Discussionsupporting
confidence: 76%
“…For example, decadal variations in pan evaporation and sunshine duration measurements provide independent indication for dimming and subsequent brightening in various regions of the globe, such as in Europe, China, the former Soviet Union, South America, New Zealand, and on Pacific islands (Roderick and Farquhar 2002;Qian et al 2006;Sanchez-Lorenzo et al 2008, 2009Liley 2009;Raichijk 2011). The widely available data on the diurnal temperature range (DTR; the difference between daily maximum and minimum temperature) were shown to contain information on decadal changes in SSR, as they allow us to disentangle the solar (daytime) and thermal (nighttime) surface radiative heating (Liu et al 2004;Makowski et al 2009;Ye et al 2010). Terrestrial DTR observations display overall a distinct decrease from the 1950s to the 1980s caused by a decline in daily maximum temperatures, which are particularly affected by SSR dimming ).…”
Section: What Observations Tellmentioning
confidence: 99%
“…These instruments included the Yanishevsky thermoelectric pyranometer for measuring SSR and diffuse solar radiation (DfSR) and the Yanishevsky thermoelectric actinometer for measuring direct solar radiation (DiSR) (Xia, 2010a;Ye et al, 2010;Tang et al, 2011), with respective error estimates of ≤5 % and ≤3 % . China started making its own instruments after 1993 and replaced the SSR/DfSR recorders with the DFY-4 pyranometer and the DiSR recorder with the DFY-3 pyrheliometer (Xia, 2010a;Ye et al, 2010;Tang et al, 2011), with errors not exceeding 5 % and 2 %, respectively . Data recorded by the instruments are governed by China Meteorological Administration (CMA) and are available at China Meteorological Data Sharing Service System (CMDS, http://cdc.cma.gov.cn/).…”
Section: Dimming and Brightening In Surface Solar Radiationmentioning
confidence: 99%