Young precariat at the forefront: anti-nuclear rallies in post-Fukushima Japan     

Chizuko UENO 《Inter-Asia Cultural Studies》2013,14(2):317-324

Japan suffered a catastrophic disaster on March 11, 2011. The earthquake, tsunami, and nuclear radiation leakage from the Fukushima Daiichi nuclear power plant devastated the northeastern part of the country and threatened the entire country and beyond with the risk of radiation. Nowadays, movements against nuclear power plants are emerging across the country. The crisis indeed provides a chance for Japan to forge a new energy policy. However, the activists' claims are not narrowly limited to such energy issues. They call for a fundamentally fairer society and propose alternative ways of life, regarding nuclear power plants as symbols supporting the economic development that Japan enjoyed over the post-Second World War period. As an ethnography, this paper documents the 60,000-citizen Goodbye Nuclear Power Plants (Sayonara Genpatsu) rally that mobilized in central Tokyo on September 19, 2011, as well as the Occupy Tokyo action on October 15, 2011 Occupy Tokyo オキュパイ東京. 2011. “Occupy Tokyo, the Rally and Demonstration in Shinjuku” “オキュパイ東京新宿の集会とデモ.” YouTube video, 9:19, from a demonstration recorded on October 15 and posted on October 17, done by Shinya Adachi. http://youtube/FoKkhRAkwJU  [Google Scholar], presenting the real voices of the rally participants against nuclear power. In particular, I will focus on the voices of young precariat participants, the major actors in the anti-nuclear rally who were generated from and revealed as the negative result of Japan's neoliberal economic policy, held since the 2000s. Further, I argue that their mounting anger might be a trigger for new post-neoliberal politics in post-Fukushima Japan.  相似文献   

青藏高原唐古拉山北坡D105点土壤温度的时间序列分析   总被引：1，自引：0，他引：1  

杨梅学姚檀栋 《资源科学》2000,22(2):77-80

通过对位于唐古拉山北坡的D105点不同尝试土壤温度时间序列的分析,表明各层日平均土壤温度的时间变化具有很好的年周期,其变化曲线为－正弦曲线。浅层土壤温度的波动比其较深层土壤温度的波动大,但对同一层而言,其波动程度尽管在夏半年略大于冬半年,但差别不大。地表、0.05m和0.2m深处,土壤日最高温度的变化幅度要明显大于最低温的变化幅度;同时,日最高温与日最低温的变化趋势并不完全一致。积雪可能对土壤日最高温、日最低温和日温差有较大影响。地表1a中的最大日温差可达60.4℃（1998年3月27日）,1a中极端日最高温度可达39.7℃,最低湿达－16.5℃。夏半年日温差明显大于冬半年,且日温差随深度的增加而减小,到80cm深处已基本上看不到明显的日温差。  相似文献   

1998年夏季（7，8月）藏北降水的某些特征分析   总被引：2，自引：0，他引：2  

杨梅学姚檀栋  Ken’ichi UENO 《资源科学》2000,22(6):43-45

利用GAME-Tibet加强观测期间所得到的青藏高原不同地点的降水量资料,初步分析了1998年7月和8月夏降风降水随纬度和海拔高度的变化特征。研究表明藏北高原夏季风降水的分布是纬度效应和海拔高度效应综合作用的结果。7月份降水量的纬度效应要比高度效应明显,而8月份的降水量不但具有一定的纬度效应,也具有一定的海拔高度效应。7月∽8月份的降水量主要表现为随纬度的分布特征,但它也受到海拔高度效应的修正,即由于地形对降水的再分配过程,使得某些测点降水随海拔高度的升高而增加。由于青藏高原地表状况复杂,其上的降水显然应当同时受到各种因素的影响和制约,因此要简单地区分各因子的作用是较困难的。  相似文献