行星边界层内的城市热岛效应对热浪的响应以及上海上空水平对流的影响

IF 4.5 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES Atmospheric Research Pub Date : 2024-10-10 DOI:10.1016/j.atmosres.2024.107721
Jialing Xin , Yuanjie Zhang , Weihua Bai , Zhaokai Song
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引用次数: 0

摘要

本研究描述了行星边界层(PBL)内城市热岛(UHI)的变化特征,并基于数值模式模拟研究了2019年8月上海市上空热浪(HW)事件中水平对流对UHI变化的影响。研究发现,在热浪条件下,UHI 加剧,UHI 强度从地表向上逐渐减弱。HW期间,地表、近地面和PBL的昼间UHI分别比HW前高3.68 K(29.27%)、1.41 K(33.52%)和1.04 K(36.97%),而夜间UHI至少在此情况下对HW无明显响应。降温期间,地表、近地表(2 米)和后海湾的平均 UHI 分别为白天 6.83 K(2.68 K)、2.45 K(1.34 K)和 1.73 K(0.04 K)。一般来说,PBL UHI 只存在于白天,可能是由热对流扩散引起的。近地面和后海平面超高气温影响受水平对流的影响较大,导致不同方向的农村地区超高气温强度和变化不同。在沿江(沿海)农村地区,来自长江(海洋)的冷平流导致了巨大的 UHI 增强,而城市地区的强冷平流则很好地解释了 UHI 的快速减弱。这项研究强调,除了局地热力因素外,同步环流也在超高温影响和高湿度事件之间的相互作用中发挥了重要作用。
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Response of urban heat island effects within the planetary boundary layer to heat waves and impact of horizontal advection over Shanghai
This study characterizes the variation of the urban heat island (UHI) within the planetary boundary layer (PBL) and investigates the horizontal advection effects on the UHI variation throughout a heat wave (HW) event over Shanghai municipality in August 2019 based on numerical model simulations. It is found that the UHI intensifies under HW conditions with the UHI intensity gradually weakening from the surface upwards. The daytime UHIs during the HW are 3.68 K (29.27 %), 1.41 K (33.52 %) and 1.04 K (36.97 %) higher than those during the pre-HW at the surface, near-surface and in the PBL, respectively, while the nighttime UHIs have no significant response to the HW at least for this case. The mean UHIs during the HW period at the surface, near-surface (2 m) and in the PBL are 6.83 K (2.68 K), 2.45 K (1.34 K), and 1.73 K (0.04 K) in the daytime (nighttime), respectively. The PBL UHI generally exists only in the daytime potentially caused by the thermal convective diffusion. The near-surface and PBL UHIs are significantly affected by the horizontal advection, resulting in different UHI intensities and variations against rural regions in different orientations. Cold advection from the Yangtze River (the ocean) in the riverside (coastal) rural region corresponds to the great UHI intensification, while the strong cold advection in the urban region well explains the fast UHI weakening. This study highlights that, besides local thermal factors, synoptic circulation also play an important role in the interaction between the UHI effect and HW events.
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来源期刊
Atmospheric Research
Atmospheric Research 地学-气象与大气科学
CiteScore
9.40
自引率
10.90%
发文量
460
审稿时长
47 days
期刊介绍: The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.
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