Page 194 - 《高原气象》2026年第1期
P. 194

高     原      气     象                                 45 卷
              190





                         Study on the Impact of Urbanization on Summer Heat Waves

                                                in Yangtze River Delta


                                     WU Yujia 1, 2, 3 , LI Yarong , HE Jianjun , CHEN Liang 1, 2
                                                                       3
                                                           3, 4
                (1. Key Laboratory of Geographic Information Science(Ministry of Education), East China Normal University, Shanghai  200241, China;
                               2. School of Geographic Sciences, East China Normal University, Shanghai  200241, China;
                             3. State Key Laboratory of Severe Weather Meteorological Science and Technology, Chinese Academy
                                            of Meteorological Sciences, Beijing  100081, China;
                            4. College of Earth and Environmental Sciences, Lanzhou University, Lanzhou  730000, Gansu, China)

             Abstract: Under the background of global climate warming and rapid urbanization, extreme heat events have be‐
             come a significant threat to human health and social sustainable development, particularly in Yangtze River Delta
             (YRD), a densely populated and economically developed region. Based on meteorological observations from
             1961 to 2020, this study systematically analyzes the trends of daily maximum temperature, daily mean tempera‐
             ture, and heat wave indices in the YRD. Additionally, sensitivity experiments using the WRF model are conduct‐
             ed to assess the impact of urban land use on extreme high temperature events. The results show that: (1) Both
             daily maximum temperature and daily mean temperature in the YRD have exhibited significant upward trends
             over the past few decades, with the increase in daily maximum temperature [0. 194 ℃·(10a)] being more pro‐
                                                                                              -1
                                                                   -1
             nounced than that in daily mean temperature [0. 187 ℃·(10a)]. Pettitt test results indicate a significant change
             point in 1993, with temperatures showing a downward trend before the change point and shifting to an upward
             trend  after  the  change  point.(2) The  frequency,  duration,  and  intensity  of  heat  waves  have  significantly  in‐
                                                                                -1
                                                                                       -1
             creased at rates of 0. 190 time·(10a) , 0. 475 d·(10a)  and 0. 772 ℃·time ·(10a) , respectively, indicating
                                              -1
                                                              -1
             that the frequency, duration and intensity of heat waves increased significantly. The change point for heat wave
             indices lags behind that of temperature change point and occurring in 2000. It showed an insignificant downward
             trend before the change point, and turning into a significant upward trend after the change. Intensity of heat wave
             increasing at a much higher rate than frequency and duration.(3) Urbanization has a significant impact on tem‐
             perature  and  heat  waves. The  daily  maximum  temperature [0. 243  ℃·(10a)]  and  daily  mean  temperature
                                                                                  -1
                             -1
                                                                                                            -1
             [0. 261 ℃·(10a)] of urban stations being significantly higher than those of rural stations [0. 171 ℃·(10a) 、
             0. 167 ℃·(10a)], suggesting that urbanization has an amplifying effect on warming. The increasing trends of
                            -1
             heat wave indices at urban stations are also significantly stronger than those at rural stations, indicating that ur‐
             banization may enhance the occurrence of heat waves.(4) The WRF model can effectively simulate the hourly
             variation of temperature, and urban land use significantly affect urban station temperatures, especially during hot
             days, with a more pronounced effect at night. Urban underlying surfaces enhance the surface energy changes of
             urban stations during hot days by changing the surface energy budget (such as sensible heat flux, latent heat flux
             and surface heat storage), which intensifies the temperature during hot days, while rural stations are less affect‐
             ed by urbanization. This indicates that the urbanization process has a more obvious impact on extreme high tem‐
             perature events in urban areas. The frequency, intensity and duration of heat waves in the Yangtze River Delta re‐
             gion have shown a significant upward trend in the past few decades, and urbanization has played an important
             amplifying  role  in  this. With  the  further  development  of  urbanization,  the  frequency  and  intensity  of  extreme
             high temperature events are likely to increase further, highlighting the necessity of developing effective adapta‐
             tion strategies and mitigation measures.
             Key words: WRF; urbanization; underlying surface; heat waves; Yangtze River Delta
   189   190   191   192   193   194   195   196   197   198   199