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一类有界捕食-食饵系统持久性的平均化条件(英文)
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作者 樊永红 王琳琳 《应用数学》 CSCD 北大核心 2017年第2期409-414,共6页
通过对解的一致上下界的估计,得到一类具有II类功能性反应的有界系统持久性的平均化条件.结果表明有界系统和它对应的平均化系统在某种程度上具有相似的性质.这就在周期系统及其对应的有界系统之间架起了一座桥梁.
关键词 有界系统 持久性 平均化条件 上下平均
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Potential Reproductive Activity of Callosobruchus subinnotatus Pic. (Coleoptera: Bruchinae), Bambara Groundnut (Vigna subterranea Verd.) Depredator
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作者 Seth Wolali Nyamador] Abla Dela Mondedji +2 位作者 Guillaume Koffivi Ketoh Komina Amevoin Isabelle Adole Glitho 《Journal of Life Sciences》 2016年第3期134-144,共11页
Callosobruchus subinnotatus Pic. (Coleoptera: Bruchinae) is the most important depredator of Bambara groundnut seeds (Vigna subterranea Verd.) in West Africa. In view of an efficient control of its populations, s... Callosobruchus subinnotatus Pic. (Coleoptera: Bruchinae) is the most important depredator of Bambara groundnut seeds (Vigna subterranea Verd.) in West Africa. In view of an efficient control of its populations, some of the biological parameters of C. subinnotatus were determined under laboratory conditions (30 ± 2℃; 72 ± 2% HR; 12h: 12h LD). The results have shown that the mean lifespan of females (11.36±1.85 days) is shorter than that of males (15.14 ±2.4 days). The female lays 80.83% eggs within the first 6 days after her emergence with a mean fecundity of 121.34 ±27.62 eggs. The means egg fertility, survival and adult emergence rates are respectively 96.19±1.45%, 97.72 ± 1.08% and 94.01± 2.14%. The sex ratio is in favor of males with a mean of 0.845 ± 0.08. The monitoring of adult emergence in connection with their reproductive status showed that the offspring of C. subinnotatus consists of two physiotypes, a reproductive type that appears during the first 8 days of emergence with a short development time (28.35± 3.36 days) and a non reproductive type that appears from the 9th day of emergence with a longer development time (37.92 ± 3.92 days). 展开更多
关键词 Callosobruchus subinnotatus Vigna subterranea biological parameters physiotypes.
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A high resolution simulation of climate change over China 被引量:42
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作者 GAO XueJie SHI Ying Filippo GIORGI 《Science China Earth Sciences》 SCIE EI CAS 2011年第3期462-472,共11页
Multi-decadal high resolution climate change simulations over East Asia were performed by using The Abdus Salam International Centre for Theoretical Physics (ICTP) Regional Climate Model (RegCM3), nested within the NA... Multi-decadal high resolution climate change simulations over East Asia were performed by using The Abdus Salam International Centre for Theoretical Physics (ICTP) Regional Climate Model (RegCM3), nested within the NASA/NCAR global model FvGCM/CCM3. Two sets of simulations were conducted at 20-km grid spacings, one for present day (1961-1990) and one for the future climate (2071-2100, IPCC A2 scenario). Simulations of present climate conditions over China by RegCM3 and FvGCM were compared against observations to assess the model performance. Results showed that both models repro- duced the observed spatial structure of 500 hPa height, surface air temperature and precipitation. Compared with FvGCM, RegCM3 provided increasing spatial detail of surface variables. Furthermore, RegCM3 improved the simulation of monsoon precipitation over the region. Changes in the mean temperature and precipitation were analyzed and compared between the two models. Significant warming in the end of the 21st century was simulated by both models in December-January-February (DJF), June-July-August (JJA), and the annual mean. In DJF, greater warming was simulated by FvGCM over Northeast and Northwest China, as well as the Tibetan Plateau, compared with RegCM. In JJA, RegCM3 simulated greater warming over northern China, Inner Mongolia, Northwest China, and the Tibetan Plateau. Simulated changes in DJF precipitation showed similar spatial patterns between the two models. In JJA, while FvGCM projected a prevailing increase of monsoon precipitation over China, which is in agreement with other global models, RegCM3 projected extended areas of decreased precipitation. Changes in the variability for annual mean temperature and precipitation also are presented. 展开更多
关键词 climate change regional climate model China
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