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961.
962.
963.
Zhigang Zeng Qiaoyun Wang Xiaomei Wang Shuai Chen Xuebo Yin Zhaoxue Li 《Journal of Earth System Science》2012,121(5):1317-1336
964.
965.
966.
形变仪器影响观测质量因素 总被引:1,自引:2,他引:1
通过对泰安地震台形变仪器观测资料质量的统计分析,发现影响观测质量的主要因素包括:观测环境的改善、优化可以提高观测精度;仪器管理和数据处理水平可以影响数据精度;降雨、吸潮等可以对曲线趋势变化造成影响;环境恶化,如外界抽水等干扰,会使曲线日变固体潮失真,从而掩盖真实的地壳信息。 相似文献
967.
Wang Jianglin Yang Bao Zheng Jingyun Zhang Xuezhen Wang Zhiyuan Fang Miao Shi Feng Liu Jingjing 《中国科学:地球科学(英文版)》2020,63(8):1126-1143
The temperature variability over multidecadal and longer timescales(e.g., the cold epochs in the late 15 th, 17 th, and early 19 th centuries) is significant and dominant in the millennium-long, large-scale reconstructions and model simulations;however, their temporal patterns in the reconstructed and simulated temperature series are not well understood and require a detailed assessment and comparison. Here, we compare the reconstructed and simulated temperature series for the Northern Hemisphere(NH) at multidecadal and longer-term timescales(30 years) by evaluating their covariance, climate sensitivity and amplitude of temperature changes. We found that covariances between different reconstructions or between reconstructions and simulations are generally high for the whole period of 850–1999 CE, due to their similar long-term temporal patterns. However,covariances between different reconstructions or between reconstructions and simulations steadily decline as time series extends further back in time, becoming particularly small during Medieval times. This is related to the large uncetainties in the reconstructions caused by the decreased number of proxy records and sample duplication during the pre-instrumental periods.Reconstructions based solely on tree-ring data show higher skill than multiproxy reconstructions in capturing the amplitude of volcanic cooling simulated by models. Meanwhile, climate models have a shorter recovery(i.e., lag) in response to the cooling caused by volcanic eruptions and solar activity minima, implying the lack of some important feedback mechanisms between external forcing and internal climate processes in climate models. Amplitudes of temperature variations in the latest published tree-ring reconstructions are comparable to those of the multiproxy reconstructions. We found that the temperature difference between the Medieval Climate Anomaly(950–1250 CE) and the Little Ice Age(1450–1850 CE) is generally larger in proxybased reconstructions than in model simulations, but the reason is unclear. 相似文献
968.
Qingsong Wang Xueliang Yuan Chunyuan Ma Zhen Zhang Jian Zuo 《Stochastic Environmental Research and Risk Assessment (SERRA)》2012,26(3):443-450
A new concept of urban environmental entropy was introduced to investigate the effect of urbanization on air environment considering
the fact that rapid development of urbanization may have negative influence on the whole air environment system. The urban
environmental entropies which were built based on the generalized thermodynamic entropy and the generalized statistic entropy,
respectively. These two entropy models have been used to analyze the relationship between the development of urbanization
and air environment. The negative entropy flow mechanism was proposed to reveal the advantages and approaches of regional
cities in improving air environment system. A case study on 17 cities in Shandong Province of China showed that the values
of urban environmental entropy were negative in most cities from 2001 to 2008, which implies that there is a positive correlation
between the development of urbanization and air environment and that is a negative entropy development level in Shandong Province
of China. In 2008, the urbanization of Qingdao city and Jinan city improved their air environments. Moreover, restraints for
both cities in air environment improvement were recognized according to the analysis of negative entropy flow mechanism. 相似文献
969.
970.
Sensitivity of hydrological variables to climate change in the Haihe River basin,China 总被引:1,自引:0,他引:1
Zhenxin Bao Jianyun Zhang Jiufu Liu Guoqing Wang Xiaolin Yan Xiaojun Wang Liru Zhang 《水文研究》2012,26(15):2294-2306
Using the defined sensitivity index, the sensitivity of streamflow, evapotranspiration and soil moisture to climate change was investigated in four catchments in the Haihe River basin. Climate change contained three parts: annual precipitation and temperature change and the change of the percentage of precipitation in the flood season (Pf). With satisfying monthly streamflow simulation using the variable infiltration capacity model, the sensitivity was estimated by the change of simulated hydrological variables with hypothetical climatic scenarios and observed climatic data. The results indicated that (i) the sensitivity of streamflow would increase as precipitation or Pf increased but would decrease as temperature increased; (ii) the sensitivity of evapotranspiration and soil moisture would decrease as precipitation or temperature increased, but it to Pf varied in different catchments; and (iii) hydrological variables were more sensitive to precipitation, followed by Pf, and then temperature. The nonlinear response of streamflow, evapotranspiration and soil moisture to climate change could provide a reference for water resources planning and management under future climate change scenarios in the Haihe River basin. Copyright © 2011 John Wiley & Sons, Ltd. 相似文献