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海南岛土地覆盖变化对海风锋结构演变影响的数值模拟

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本文利用WRF-Noah陆气耦合中尺度模式,针对海南岛一次典型的海风锋事件进行了高分辨率的数值模拟,研究了海南岛土地覆盖(下垫面)变化对海风锋结构演变的影响及其机制.结果表明,海南岛土地覆盖变化对海风锋的作用是通过多种地表和植被属性的综合影响决定的.森林化试验中动力和热力作用分别抑制和促进海风锋的发展,对海风锋的影响是两者共同作用的结果;反照率的减小引起净辐射的增大,从而使感热通量小幅增加,使低层大气增温而增加海陆温度梯度,这在一定程度上增强了海风驱动力,但地表粗糙度的增大减弱了海风风速,进一步减弱了海风锋传播距离和上升速度.然而,由于海南岛森林覆盖面积较大,导致森林化试验与控制试验中海风锋的整体差异较小.相比之下,荒漠化试验中热力和动力作用均有利于海风锋的发展;反照率的增大和叶面积指数的降低,改变了地表能量分配,造成潜热通量显著减小,感热通量先减少后增大,对低层大气的增温效应非常明显,从而加大了海陆温度梯度.另一方面,地表粗糙度显著减小,下垫面对海风的阻挡作用减弱,海风风速增大.因此,荒漠化试验海风锋传播距离、上升速度以及海风厚度都显著增大.
Numerical Study of the Impact of Land Cover Change on Structure and Evolution of the Sea Breeze Front over Hainan Island
The sea breeze front(SBF)is the landward edge of the sea breeze circulation,which has characteristics similar to the cold front.SBF is a key object of coastal meteorological research because it can trigger strong convection even in disastrous weather,such as thunderstorms in coastal areas.Herein,a typical SBF over Hainan Island is examined using the weather research and forecasting model.Sensitive experiments were designed to explore the effect of land cover changes on the structure and evolution of SBF and its possible mechanism.Results revealed that the effect of land cover change on SBF is determined by the comprehensive influence of multiple surface and vegetation attributes.The dynamic effects of afforestation inhibit the development of SBF,while the thermal effects promote it,which means that the influence of afforestation on SBF is because of the competition between two opposite forces.The decreased albedo and increased leaf area index result in a small increase in sensible heat fluxes,which can increase the temperature difference between land and sea—the driving force of sea breeze.The increase in surface roughness can decrease the wind speed,inland propagation,and vertical velocity of SBF.However,the difference in SBF between the FOREST and CNTL experiments is small due to the large forest land use of Hainan Island.Meanwhile,the thermal and dynamic effects of deforestation are beneficial in promoting the development of SBF.The increased albedo and decreased leaf area index result in a significant decrease in latent heat flux and an increase in sensible heat flux in the afternoon.Thus,the warming and humidification effects of deforestation on the lower atmosphere are obvious,which increases the sea-land temperature gradient.Meanwhile,the decrease in surface roughness causes an increase in the wind speed.Consequently,the wind speed,inland propagation,and vertical velocity of SBF are significantly increased.

Sea breeze frontLand cover changeForestationDesertificationTropical island

依斯拉木·吾拉音、苗峻峰、吴冰雪

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南京信息工程大学大气科学学院,南京 210044

海南省南海气象防灾减灾重点实验室,海口 570203

中国气象局乌鲁木齐沙漠气象研究所,乌鲁木齐 830002

海南省气象台,海口 570311

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海风锋 土地覆盖变化 森林化 荒漠化 热带岛屿

海南省南海气象防灾减灾重点实验室开放基金项目

SCSF201903

2024

大气科学
中国科学院大气物理研究所

大气科学

CSTPCD北大核心
影响因子:2.11
ISSN:1006-9895
年,卷(期):2024.48(2)
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