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Spatiotemporal variability and climate forcing mechanisms

                1. Introduction                                     climate-driving mechanisms underlying the significant
                                                                    decline in WER and SER from the perspective of climate
                Against the  backdrop  of intensifying  global  climate   change. This study aims to answer two key questions:
                change, China has formally announced its “Dual Carbon   (i) what are the temporal and spatial evolution patterns
                Goals” (peaking carbon emissions by 2030 and achieving   of WER and SER under the background of a warm and
                carbon neutrality by 2060), prioritizing energy structure   humid climate in NWC? and (ii) What are the climate-
                transformation  through accelerated  clean energy   driving  mechanisms  of  the  WER  and  SER  in  NWC
                adoption and phased fossil fuel reduction.  As  two   changes on an interannual scale in NWC?
                                                       1-4
                technologically mature and globally scalable renewable
                energy sources, wind and solar power have undergone   2. Materials and methods
                rapid deployment in China’s energy matrix.  Notably,
                                                       5-7
                these climate-dependent  resources exhibit strong   2.1. Study area
                spatiotemporal  variability  influenced  by  atmospheric   NWC is an important part of the arid region of Central
                dynamics and surface–atmosphere interactions. 8,9   Asia (73°25’ – 110°55’E, 31°35’ – 49°15’N), accounting
                  Meteorological  records  over  the  past  five  decades   for about one-third  of China’s land area  (Figure  1).
                reveal  concerning  trends:  A  persistent  decline  in   The  region  is deeply  inland,  far from the  ocean,  and
                terrestrial  wind speeds and diminishing annual     surrounded by high mountains, which block the inflow
                total solar radiation (TSR) across mainland China,   of moist oceanic air. It exhibits a typical continental
                with  particularly  marked  reductions  in northwest   climate and is thus the driest area in China. 16,17  Although
                China (NWC).   While urbanization-induced surface   the region is rich in WER and SER, and the climate has
                              8
                modifications (such as increased albedo and aerodynamic   shown a trend of warming and humidification in recent
                roughness) are recognized contributing factors, NWC   decades, both WER and SER in the region have been
                presents a counterintuitive  case study. 10,11  This  region   gradually decreasing. 18,19
                has maintained relatively  stable urbanization  levels
                since 1987 while experiencing a paradoxical “warm–  2.2. Data sources
                wet transition” climate shift.  This decoupling suggests   Daily sunshine duration, average wind speed, and
                                         12
                that synoptic-scale  circulation  changes may dominate   average air pressure data were obtained from the China
                over local anthropogenic impacts in driving renewable   Surface Climate Data Daily Value Dataset V3.0. In this
                energy resource depletion in NWC. 12,13             study, data pre-processing was conducted by discarding
                  Present research paradigms exhibit  two critical   sites with significant data loss. The exclusion criterion
                limitations:  (i) overemphasis  on continental/global-  was that sites with more than 20% missing data over
                scale analyses, which obscures regional  climate  zone   the time series were removed. For stations with <20%
                specificities,  particularly  in  arid  regions  with  optimal   missing data, linear interpolation was performed using
                renewable  energy  resource  development  potential;    data from adjacent years. The interpolated results were
                                                               5,6
                and  (ii) methodological  constraints  that  favor  short-  then compared with and corrected using the climatic
                term (<10 years) observational datasets over decadal-  research unit (CRU) dataset. After this pre-processing,
                scale climate pattern analyses, 9,10  while also neglecting   a total  of 400 meteorological stations  with complete
                differences  across  climate  zones,  especially  in  arid   sunshine duration and average wind speed data from
                areas where the wind energy resources (WER) and     1961 to 2019 were selected.
                solar energy resources (SER) are  abundant  and        In addition, to explore the climate-driving
                conditions for their development  and utilization  are   mechanisms behind WER and SER in NWC, relevant
                more favorable. 14,15  Addressing these knowledge gaps is   data on atmospheric  circulation  (ASC)  and climate
                imperative  for developing  climate-resilient  renewable   change were collected  based on existing research.
                energy strategies in vulnerable ecotones.           The ASC index data were sourced from the National
                  In summary, to explain the significant decline in WER   Oceanic  and Atmospheric Administration,  United
                and SER in NWC over the past half century, this study   States  of  America  (http://www.esrl.noaa.gov/psd/
                takes NWC as the study area and applies trend analysis,   enso/). To supplement climate indicators such as cloud
                spectral analysis, and random forest (RF) modeling to   cover, the study also utilized CRU’s 100-year sequence
                examine the evolution characteristics of WER and SER   grid dataset (http://www.cru.uea.ac.uk/data/). The time
                in NWC from 1961 to 2019. It further  analyzes  the   series for all the above data spans from 1961 to 2019.




                Volume 22 Issue 4 (2025)                        29                           doi: 10.36922/AJWEP025190147
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