地理科学进展 ›› 2015, Vol. 34 ›› Issue (8): 1061-1071.doi: 10.18306/dlkxjz.2015.08.013
• 水文与气候 • 上一篇
胡文峰1(), 王乃昂1,2*(
), 赵力强1, 宁凯1, 张洵赫1, 孙杰1
出版日期:
2015-08-25
发布日期:
2015-08-25
作者简介:
作者简介:胡文峰(1978-),男,安徽太湖县人,博士研究生,主要从事湍流与通量研究,E-mail:
基金资助:
HU Wenfeng1(), WANG Nai'ang1,2,*(
), ZHAO Liqiang1, NING Kai1, ZHANG Xunhe1, SUN Jie1
Online:
2015-08-25
Published:
2015-08-25
Contact:
WANG Nai'ang
摘要:
利用2012年8月-2013年7月在巴丹吉林沙漠腹地典型湖泊上用涡动相关系统观测的湍流资料,分析了湍流方差统计特征、微气象特征,计算了湍流热通量和湖泊蒸发量,初步结论为:①湖面上局地环流复杂,湍流三维风速的标准差与稳定度(Z/L)之间满足1/3次律。②湖面辐射分量具有明显季节变化和日变化特征,结冰期和非结冰期能量分配不同,冬季湖泊将储存的能量向大气传递;潜热通量和感热通量季节变化存在差异,但均有明显的昼夜变化特征。③湖气界面的感热通量在不同的月份也存在差异,感热以湖泊向大气传递为主;潜热通量夏半年远大于冬半年,在一天中6:00-8:00时处于最低值,15:00-16:00时达到峰值,在冬季会出现潜热向下输送现象。感热通量和潜热通量日变化呈负相关,湖面有效能量主要分配给潜热,湖泊同周围环境以水汽交换为主。④湖面平均蒸发速率为3.97 mm/d,累计蒸发量为1450±10 mm/a,同期的蒸发量是降水量的20多倍,湖泊主要靠地下水补给。这些结论可为进一步研究巴丹吉林沙漠腹地湖泊群的水循环及补给来源提供参考。
胡文峰, 王乃昂, 赵力强, 宁凯, 张洵赫, 孙杰. 巴丹吉林沙漠典型湖泊湖气界面水一热交换特征[J]. 地理科学进展, 2015, 34(8): 1061-1071.
HU Wenfeng, WANG Nai'ang, ZHAO Liqiang, NING Kai, ZHANG Xunhe, SUN Jie. Water-heat exchange over a typical lake in Badain Jaran Desert, China[J]. PROGRESS IN GEOGRAPHY, 2015, 34(8): 1061-1071.
表1
观测仪器类型"
主要观测指标 | 传感器名称 | 仪器公司/型号 | 技术指标 |
---|---|---|---|
CO2/H2O密度 | CO2/H2O分析仪 | LI-COR/LI-7500A | 工作温度:-25℃~+50 ℃;精度:±1%;零点偏移:0.01 ppm-CO2,±0.03 ppt-H2O。 |
三维风速和虚温 | 三维超声风速仪 | GILL/R3-50 | 工作温度:-40 ℃~+60 ℃;精度:±0.5%;分辨率:0.01 m/s。 |
空气温度/相对湿度 | 温湿传感器 | Vaisala/HMP155 | 测量范围:-40 ℃~+60 ℃;精度:(±1% T)/(±2% RH)。 |
水面红外辐射温度 | 温度传感器 | Apogee/SI-111 | 工作温度:-55℃~+80 ℃;精度:±0.2 ℃。 |
辐射 | 四分量辐射传感器 | Hukseflux/NR01 | 工作温度:-40℃~+80 ℃;热偏移:<15 W/m2;精度:±1%。 |
降水量 | 雨量筒 | Onset/HOBO RG3-M | 分辨率:0.2 mm/斗。 |
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