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　(　)　(　)通(tong)报(bao)称(cheng)，(，)马(ma)林(lin)严(yan)重(zhong)违(wei)反(fan)党(dang)的(de)政(zheng)治(zhi)纪(ji)律(lv)、(、)中(zhong)央(yang)八(ba)项(xiang)规(gui)定(ding)精(jing)神(shen)、(、)组(zu)织(zhi)纪(ji)律(lv)、(、)廉(lian)洁(jie)纪(ji)律(lv)、(、)工(gong)作(zuo)纪(ji)律(lv)和(he)生(sheng)活(huo)纪(ji)律(lv)，(，)违(wei)反(fan)国(guo)家(jia)法(fa)律(lv)法(fa)规(gui)，(，)构(gou)成(cheng)严(yan)重(zhong)职(zhi)务(wu)违(wei)法(fa)并(bing)涉(she)嫌(xian)犯(fan)罪(zui)，(，)且(qie)在(zai)党(dang)的(de)十(shi)八(ba)大(da)后(hou)仍(reng)不(bu)收(shou)敛(lian)、(、)不(bu)收(shou)手(shou)，(，)性(xing)质(zhi)严(yan)重(zhong)，(，)影(ying)响(xiang)恶(e)劣(lie)，(，)应(ying)予(yu)严(yan)肃(su)处(chu)理(li)。(。)依(yi)据(ju)《(《)中(zhong)国(guo)共(gong)产(chan)党(dang)纪(ji)律(lv)处(chu)分(fen)条(tiao)例(li)》(》)《(《)中(zhong)华(hua)人(ren)民(min)共(gong)和(he)国(guo)监(jian)察(cha)法(fa)》(》)《(《)中(zhong)华(hua)人(ren)民(min)共(gong)和(he)国(guo)公(gong)职(zhi)人(ren)员(yuan)政(zheng)务(wu)处(chu)分(fen)法(fa)》(》)等(deng)有(you)关(guan)规(gui)定(ding)，(，)经(jing)云(yun)南(nan)省(sheng)纪(ji)委(wei)常(chang)委(wei)会(hui)会(hui)议(yi)研(yan)究(jiu)并(bing)报(bao)云(yun)南(nan)省(sheng)委(wei)批(pi)准(zhun)，(，)决(jue)定(ding)给(gei)予(yu)马(ma)林(lin)开(kai)除(chu)党(dang)籍(ji)处(chu)分(fen)；(；)按(an)规(gui)定(ding)取(qu)消(xiao)其(qi)享(xiang)受(shou)的(de)待(dai)遇(yu)；(；)收(shou)缴(jiao)其(qi)违(wei)纪(ji)违(wei)法(fa)所(suo)得(de)；(；)将(jiang)其(qi)涉(she)嫌(xian)犯(fan)罪(zui)问(wen)题(ti)移(yi)送(song)检(jian)察(cha)机(ji)关(guan)依(yi)法(fa)审(shen)查(zha)起(qi)诉(su)，(，)所(suo)涉(she)财(cai)物(wu)一(yi)并(bing)移(yi)送(song)。(。)∪▂∪∪０∪∪　　duiyuriben，zhongfangfachudexinxifeichangmingque，zuochudefanyingfeichangjianjue。zhongfangqianglieduncurifangkeshouzhongrisigezhengzhiwenjianyuanzehezaitaiwanwentishangsuozuozhengzhichengnuo，tingzhiganshezhongguoneizheng，shenzhongtuoshanchulishetaiwenti，buyaozaicuowudedaolushangyuezouyueyuan。ruguoribengenzhemeiguoyiqitiaoxinzhongguohexinliyi，nametadagailvyaochengshouzhongfanggengzhijiegengqiangdehuiji。shuojubuhaotingde，fanzhiribenyaobifanzhimeiguojiandanyixingyixie。duici，rifangbuyingyourenhejiaoxing。유　　为何隆冬时节的寒潮反而比春秋少呢？杨舒楠解释，春秋季属于季节转换时段，夏季风与冬季风切换，天气系统及冷空气活动频繁，导致气温起伏比较剧烈。尤其是秋季，前期基础温度比较高，一次冷空气开始之前往往出现明显升温，冷空气影响后降温幅度非常大，容易形成“断崖式”降温，相对容易达到寒潮标准。而隆冬时节，基础气温本来就低，冷空气来袭时降温幅度往往有限，达到寒潮标准的情况就相对较少。

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