干旱区研究 ›› 2018, Vol. 35 ›› Issue (1): 50-56.doi: 10.13866/j.azr.2018.01.07 cstr: 32277.14.AZR.20180107

• 天气与气候 • 上一篇    下一篇

青海湖流域高寒湿地光合有效辐射特征

高黎明1,2, 张乐乐1,2, 陈克龙2,3, 毛亚辉1,2   

  1. 1.青海师范大学地理科学学院, 青海 西宁 810008;
    2.青海省自然地理与环境过程重点实验室, 青海 西宁 810008;
    3.青海师范大学, 青海 西宁 810008
  • 收稿日期:2017-04-21 修回日期:2017-06-01 出版日期:2018-01-15 发布日期:2018-02-06
  • 通讯作者: 陈克龙.E-mail:ckl7813@163.com
  • 作者简介:高黎明(1986-),女,博士,讲师,主要从事生态水文过程研究. E-mail:gaogaotahj@163.com
  • 基金资助:
    青海省自然科学基金项目(2017-ZJ-951Q, 2017-ZJ-782);国家自然科学基金项目(41705139, 41661023, 41360005);“高寒环境联合监测研究云的建设与应用”项目(XXH12503-05-07)资助

Photosynthetically Active Radiation in Alpine Wetland in the Qinghai Lake Watershed

GAO Li-ming1,2, ZHANG Le-le1,2, CHEN Ke-long2,3, MAO Ya-hui1,2   

  1. 1. College of Life Science and Geography,Qinghai Normal University,Xining 810008,Qinghai,China;
    2. Qinghai Province Key Laboratory of Physical Geography and Environmental Process,Xining 810008,Qinghai,China;
    3. Science and Technology Department,Qinghai Normal University,Xining 810008,Qinghai,China
  • Received:2017-04-21 Revised:2017-06-01 Published:2018-01-15 Online:2018-02-06

摘要: 光合有效辐射(PAR)是生态系统过程中的一个重要参数,本文基于青海湖流域小泊湖和瓦颜山湿地气象站观测的辐射资料,对高寒湿地PAR变化特征进行了分析。结果表明:2个站点的太阳总辐射(Q)和PAR值都存在明显的日变化和季节变化特征,Q和PAR一日之中的最大值出现在13:00左右(北京时间),在一年中,最大值出现在6月,最小值出现在12月。光合有效辐射系数(ηPAR)也存在明显的季节变化特征,最大值出现在7月,主要与这个时期青海湖流域大气水汽含量最多有关。最后,利用瓦颜山数据基于晴空指数(Kt)和太阳总辐射(Q)构建出了一个PAR日值估算模型,并在小泊湖进行了模型的验证,结果表明本研究构建的模型能够满足不同天气条件下青海湖流域PAR的估算要求。

关键词: 总辐射, 光合有效辐射, 高寒湿地, 青海湖流域

Abstract: Photosynthetically active radiation (PAR) is an important parameter in the process of ecosystem. However,there are few reports on the change of PAR in alpine wetland. In this paper,the characteristics of PAR variation in the alpine wetland were analyzed based on the radiation data from the Xiaobohu and Wayanshan wetland meteorological stations in the Qinghai Lake Basin.The results showed that the annual global radiation (Q) and PAR at Xiaobohu Meteorological Station were 6 711.6 MJ·m-2 and 2 888.3 MJ·m-2,but they were 5 963.4 MJ·m-2 and 2 527.5 MJ·m-2 at Wayanshan Meteorological Station,respectively.The values of Q and PAR at the Wayanshan station were significantly lower than those at the Xiaobohu station.The daily and seasonal variations of both Q and PAR values at the two sites were obvious,and the maximum values of Q and PAR occurred around 13:00 o’clock.The maximum Q and PAR values appeared in June,and the minimum ones in December.The average annual photosynthetically active radiation coefficients (ηPAR) at the Xiaobohu and Wayanshan stations were 0.43 and 0.44 respectively.The seasonal variation of ηPAR at both sites was also obvious,the maximum value appeared in July,and the main reason was that the water vapor content over the Qinghai Lake Basin was the highest in July.Finally,a statistical model was developed based on the clearness index (Kt) and total solar radiation (Q) data at the Wayanshan station so as to estimate the PAR values in the whole Qinghai Lake Basin.The model was also verified at the Xiaobohu station,the results showed that the model could be used to meet the requirements of estimating the PAR values under different weather conditions in the Qinghai Lake Basin.

Key words: global radiation, photosynthetically active radiation, alpine wetland, Qinghai Lake Basin