共被期刊论文引用了3次
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| 1 | 东亚沙尘光学特性及其对辐射强迫和温度的影响显示文摘利用塔克拉玛干沙漠沙尘复折射指数数据对RegCM4-Dust耦合模式中的沙尘光学特性进行了更新,研究了东亚沙尘气溶胶光学特性对辐射强迫和温度的影响。结果表明:东亚沙尘气溶胶光学特性与模式默认值(OPAC模型)存在明显的差别,主要表现在:消光能力较弱;吸收性较弱,散射性较强;前向散射较弱,后向散射较强。2006年春季沙尘气溶胶光学厚度高值区主要位于塔克拉玛干沙漠、古尔班通古特沙漠、巴丹吉林沙漠、鄂尔多斯高原及黄土高原等地区,最大值出现在巴丹吉林沙漠。采用东亚沙尘光学模型模拟2006年春季东亚地区大气顶净强迫为-4.86 W·m-2,其中短波强迫为-5.34 W·m-2,长波强迫为0.48 W·m-2;地面净强迫为-11.23 W·m-2,其中短波强迫为-13.70 W·m-2,长波强迫为2.47 W·m-2。2006年春季沙尘气溶胶导致东亚地区整体地面降温约0.21℃,陆地上降温明显,而海洋上温度变化不明显,甚至出现升温,这样将导致海陆间热力差异的改变,从而对东亚季风环流产生影响。 | 宿兴涛 李鲲 魏强 文雯 | 2016 | 中国沙漠2016，36，5： | 10 |
| 2 | Simulation on the spatio-temporal distribution and emission flux of dust aerosol over East Asia in 2000-2009显示文摘A regional climate model (RegCM3), coupled with an online dust module, is used to simulate the spatio-temporal distribution and emission flux of dust aerosol (smaller than 20 μm in diameter) over East Asia in the period from 2000 to 2009. The model performance is firstly evaluated against available observations. Simulation results show that the model can capture the characteristics of spatio-temporal distribution of dust aerosol very well over East Asia. There always exist two extremes of dust aerosol optical depth (AOD) and column burden (CB), one is in the Taklimakan Desert of Xinjiang Uygur Autonomous Region, China, and the other is in the Badain Jaran Desert of Inner Mongolian Autonomous Region, China. The maximum value of CB appears in spring, secondary maximum in winter and minimum in autumn. To the east of 110°E, dust is transported eastward from a maximum center at a height of 700 hPa over the East Asian continent. Dust emission sources are mainly located in the Taklimakan Desert, Badain Jaran Desert, North Qinghai-Tibetan Plateau and Southwest Mongolia. There is also an obvious seasonal variation of dust emission flux (EF). Annual mean dust EF is 1,015.34 mg/(m 2 ·d), of which 62.4% and 2.3% are re-deposited onto the East Asian continent through a dry and wet deposition process, respectively, and the remaining 35.3% is injected into the atmosphere or subject to long-range transport. | XingTao Su HanJie Wang HengRui Tao LieShuang Liu HongFeng Zhang | 2013 | Research in Cold and Arid Regions2013，5，2： | 3 |
| 3 | A1B情景下东亚地区未来春季沙尘变化趋势预估显示文摘采用区域气候与沙尘耦合模式RegCM4-Dust,模拟研究了A1B情景下东亚地区未来(2015—2100年)春季沙尘变化趋势。结果表明:(1)总体上,东亚沙尘源区起尘通量与沉降通量存在明显的振荡特征,而沙尘光学厚度呈现显著的波动减小趋势;源区下游沙尘光学厚度和沉降通量均呈现显著的波动增大趋势。(2)沙尘子源区中,仅塔克拉玛干沙漠及周边地区起尘通量有显著波动减少趋势,速度达-2.1%/10a;萨雷耶西克阿特劳沙漠和呼伦贝尔沙地沙尘光学厚度减小速度最快,分别达到-2.8%/10a、-2.3%/10a。(3)未来,中国华北南部、黄淮以及长江中下游地区以及中国东、南部近海春季沙尘光学厚度增速均为1.5%/10a;中国近海沙尘沉降通量显著上升,速度达1.9%/10a。(4)地面风速尤其是最大风速变化是导致起尘通量变化的主要因素,而影响光学厚度的主要因素是地面最大风速。 | 宿兴涛 张志标 欧磊 | 2017 | 中国沙漠2017，37，2： | 2 |
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