As China＇s top leaders prepare to discuss major policies on the country＇s reform agenda during the upcoming Third Plenary Session of the 18th Communist Party of China＇s Central Committee in November 2013, the rest ...As China＇s top leaders prepare to discuss major policies on the country＇s reform agenda during the upcoming Third Plenary Session of the 18th Communist Party of China＇s Central Committee in November 2013, the rest of the world is keeping a close eye on General Secretary Xi Jinping for any clues as to the policy direction of China＇s new leadership.展开更多
In this paper, we discuss the 0, 1 distribution in the highest level sequence ae-1 of primitive sequence over Z2e generated by a primitive polynomial of degree n. First we get an estimate of the 0, 1 distribution by u...In this paper, we discuss the 0, 1 distribution in the highest level sequence ae-1 of primitive sequence over Z2e generated by a primitive polynomial of degree n. First we get an estimate of the 0, 1 distribution by using the estimates of exponential sums over Galois rings, which is tight for e relatively small to n. We also get an estimate which is suitable for e relatively large to n. Combining the two bounds, we obtain an estimate depending only on n, which shows that the larger n is, the closer to 1/2 the proportion of 1 will be.展开更多
The annual highest water level of Taihu Lake （Zm） is very significant for flood management in the Taihu Basin. This paper first describes the inter-annual and intra-annual traits of Zm from 1956 to 2000. Then, using...The annual highest water level of Taihu Lake （Zm） is very significant for flood management in the Taihu Basin. This paper first describes the inter-annual and intra-annual traits of Zm from 1956 to 2000. Then, using the Mann-Kenall （MK） and Spearman （SP） nonparametric tests, the long-term change trends of area precipitation and pan evaporation in the Taihu Basin are determined. Meanwhile, using the Morlet wavelet transformation, the fluctuation patterns and change points of precipitation and pan evaporation are analyzed. Also, human activities in the Taihu Basin are described, including land use change and hydraulic project construction. Finally, the relationship between Zm, the water level of Taihu Lake 30 days prior to the day of Zm （Z0）, and the 30-day total precipitation and pan evaporation prior to the day of Zm （P and E0, respectively） is described based on multi-linear regression equations. The relative influence of climate change and human activities on the change of Zm is quantitatively ascertained. The results demonstrate that： （1） Zm was distinctly higher during the 1980-2000 period than during the 1956-1979 period, and the 30 days prior to the day of Zm are the key phase influencing Zm every year; （2） P increased significantly at a confidence level of 95% during the 1956-2000 period, while the reverse was true for E0; （3） The relationship between Zm, P and E0 distinctly changed after 1980; （4） Climate change and human activities together caused frequent occurrences of high Zm after 1980; （5） Climate change caused a substantially greater Zm difference between the 1956-1979 and 1980-2000 periods than human activities. Climate change, as represented by P and E0, was the dominant factor raising Zm, with a relative influence ratio of 83.6%, while human activities had a smaller influence ratio of 16.4%.展开更多
The distribution of 0 and 1 is studied in the highest level ae-1, of primitive sequences over . / (2(?) ), and the upper and lower bounds on the ratio of the number of 0 to the number of 1 in one period of ae-1 are ob...The distribution of 0 and 1 is studied in the highest level ae-1, of primitive sequences over . / (2(?) ), and the upper and lower bounds on the ratio of the number of 0 to the number of 1 in one period of ae-1 are obtained. It is revealed that the larger e is, the closer to 1 the ratio will be.展开更多
文摘As China＇s top leaders prepare to discuss major policies on the country＇s reform agenda during the upcoming Third Plenary Session of the 18th Communist Party of China＇s Central Committee in November 2013, the rest of the world is keeping a close eye on General Secretary Xi Jinping for any clues as to the policy direction of China＇s new leadership.
基金This work was supported by the National Natural Science Foundation of China(Grant Nos.19971096,90104035).
文摘In this paper, we discuss the 0, 1 distribution in the highest level sequence ae-1 of primitive sequence over Z2e generated by a primitive polynomial of degree n. First we get an estimate of the 0, 1 distribution by using the estimates of exponential sums over Galois rings, which is tight for e relatively small to n. We also get an estimate which is suitable for e relatively large to n. Combining the two bounds, we obtain an estimate depending only on n, which shows that the larger n is, the closer to 1/2 the proportion of 1 will be.
基金supported by the National Key Technology R & D Program of the Ministry of Science and Technology of China (Grant No. 2006BAB14B01)the Innovation Program of Science and Technology of the Ministry of Water Resources of China (Grant No. XDS2007-04)
文摘The annual highest water level of Taihu Lake （Zm） is very significant for flood management in the Taihu Basin. This paper first describes the inter-annual and intra-annual traits of Zm from 1956 to 2000. Then, using the Mann-Kenall （MK） and Spearman （SP） nonparametric tests, the long-term change trends of area precipitation and pan evaporation in the Taihu Basin are determined. Meanwhile, using the Morlet wavelet transformation, the fluctuation patterns and change points of precipitation and pan evaporation are analyzed. Also, human activities in the Taihu Basin are described, including land use change and hydraulic project construction. Finally, the relationship between Zm, the water level of Taihu Lake 30 days prior to the day of Zm （Z0）, and the 30-day total precipitation and pan evaporation prior to the day of Zm （P and E0, respectively） is described based on multi-linear regression equations. The relative influence of climate change and human activities on the change of Zm is quantitatively ascertained. The results demonstrate that： （1） Zm was distinctly higher during the 1980-2000 period than during the 1956-1979 period, and the 30 days prior to the day of Zm are the key phase influencing Zm every year; （2） P increased significantly at a confidence level of 95% during the 1956-2000 period, while the reverse was true for E0; （3） The relationship between Zm, P and E0 distinctly changed after 1980; （4） Climate change and human activities together caused frequent occurrences of high Zm after 1980; （5） Climate change caused a substantially greater Zm difference between the 1956-1979 and 1980-2000 periods than human activities. Climate change, as represented by P and E0, was the dominant factor raising Zm, with a relative influence ratio of 83.6%, while human activities had a smaller influence ratio of 16.4%.
基金Project supported by the State Key Laboratory of Information Security,Graduate School of Chinese Academy of Sciences.
文摘The distribution of 0 and 1 is studied in the highest level ae-1, of primitive sequences over . / (2(?) ), and the upper and lower bounds on the ratio of the number of 0 to the number of 1 in one period of ae-1 are obtained. It is revealed that the larger e is, the closer to 1 the ratio will be.
