About North Asia Monitoring Solar System
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About North Asia Monitoring Solar System video introduction
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6 FAQs about [North Asia Monitoring Solar System]
How does solar radiation affect DSSR spatial variation over East Asia?
The incident solar radiation at TOA has a large influence (r2 > 0.62) on DSSR's spatial variations over East Asia in SON and DJF, while the DSSR spatial variations in MAM and JJA are mostly affected by clouds (pr2 = 0.4 to 0.7 except for NCEP-DOE in MAM).
Can machine learning estimate solar radiation across China?
The present study introduces the RF model, a popular and highly flexible machine learning algorithm, to estimate solar radiation across China at the national scale. The estimated DGSR is in good agreement with site observations across China, with mean R, RMSE, and MB values of 0.95, 2.34, and −0.04 MJ/m 2, respectively.
Do satellite-derived DSSR products show long-term trends in surface solar radiation?
In particular, changes in satellites and their orbits over time may induce spurious long-term changes that could hamper their application for assessing long-term trends in surface solar radiation [Pinker et al., 2005]. Indeed, Wild pointed out that different satellite-derived DSSR products show inconsistent trends.
How are DSSR products measured in East Asia?
Ground-based measurements from a BSRN site (Xianghe) and 94 stations from the CMA were used to evaluate the DSSR products, which were then used to quantify the DSSR spatial and seasonal variations over East Asia during July 2006 to June 2009.
Is solar radiation a topic in China?
Therefore, solar radiation is a topic that has attracted broad and increasing attention in China (Che et al., 2005; Sun et al., 2016; Li et al., 2017; Wang et al., 2016; Song et al., 2019; Tang et al., 2016, 2018; Liu et al., 2019; He & Wang et al., 2020).
What are the spatial patterns of DSSR over East Asia?
The four datasets all show similar broad spatial patterns of DSSR over East Asia, with high DSSR (180–280 Wm –2) over the Tibetan Plateau due to low cloud amount (50%) and little precipitable water (5 mm) there and low DSSR (120–200 Wm –2) over southeastern and northeastern China.