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亲子分离经历医学生防御机制和心理健康现状

中国学校卫生 2013年第2期34卷 244-245页

作者：祝亚丽张宁南京医科大学第四临床医学院江苏210029 蚌埠医学院精神医学系临床心理学教研室南京医科大学附属脑科医院

目的探讨亲子分离经历与大学生心理防御机制和心理健康之间的关系,为提高相应群体大学生的心理健康水平提供依据。方法采用防御方式问卷(DSQ)、症状自评量表(SCL-90),对蚌埠医学院随机抽取的246名有亲子分离经历者和402名无亲子分离经... 详细信息

目的探讨亲子分离经历与大学生心理防御机制和心理健康之间的关系,为提高相应群体大学生的心理健康水平提供依据。方法采用防御方式问卷(DSQ)、症状自评量表(SCL-90),对蚌埠医学院随机抽取的246名有亲子分离经历者和402名无亲子分离经历者进行问卷调查。结果有亲子分离经历组较无亲子分离经历组更多使用不成熟防御机制和中间型防御机制,差异均有统计学意义(P值均<0.05)。亲子分离年龄和持续时间对不成熟防御机制的使用均有显著影响(P值均<0.05)。不同心理健康水平有分离经历大学生在不成熟防御机制、中间型防御机制和掩饰因子使用上差异均有统计学意义(P值均<0.01)。结论亲子分离经历对大学生心理防御机制、心理健康状况会产生影响。应采取有效干预措施,促进有亲子分离经历大学生的心理健康水平。

关键词：防御机制精神卫生亲子关系学生医科

The Antarctic Oscillation-East Asian Summer Monsoon Connections in NCEP-1 and ERA-40

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Advances in Atmospheric Sciences 2009年第4期26卷 707-716页

作者：祝亚丽 Nansen-Zhu International Research Center Institute of Atmospheric Physics Chinese Academy of Sciences Graduate University of Chinese Academy of Sciences Climate Change Research Center(CCRC) Chinese Academy of Sciences

Connections between the spring Antarctic Oscillation （AAO） and the East Asian summer monsoon （EASM） in two reanalysis datasets-NCEP-1 （NCEP/NCAR Reanalysis 1） and ERA-40 （ECMWF 40- year Reanalysis）-are investigated in this study. Both show significant correlation between AAO and EASM rainfall over the Yangtze River valley, especially after about 1985. Though ERA-40 shows weaker anomalous signals connecting AAO and EASM over southern high latitudes than NCEP-1, both datasets reveal similar connecting patterns between them. A wave-train-like pattern appears in the upper levels, from southern high latitudes through east of Australia and from the Maritime Continent to East Asia. In positive AAO years, the cross equatorial southeasterly flow over the Maritime Continent in the lower levels is strengthened, the specific humidity of the whole atmosphere over East Asia increases, and convective activity is enhanced; thus the summer rainfall over East Asia increases. The spring AAO-EASM connection may be better represented in ERA-40.

关键词： Antarctic Oscillation East Asian summer monsoon NCEP-1 ERA-40

Variations of the Summer Somali and Australia Cross-Equatorial Flows and the Implications for the Asian Summer Monsoon

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Advances in Atmospheric Sciences 2012年第3期29卷 509-518页

作者：祝亚丽 Nansen-Zhu International Research Centre Institute of Atmospheric PhysicsChinese Academy of Sciences Climate Change Research Center Chinese Academy of Sciences

The temporal variations during 1948-2010 and vertical structures of the summer Somali and Australia cross-equatorial flows （CEFs） and the implications for the Asian summer monsoon were explored in this study. The strongest southerly and northerly CEFs exist at 925 hPa and 150 hPa level, respectively. The low-level Somali （LLS） CEFs were significantly connected with the rainfall in most regions of India （especially the monsoon regions）, except in a small area in southwest India. In comparison to the climatology, the low- level Australia （LLA） CEFs exhibited stronger variations at interannual time scale and are more closely connected to the East Asian summer monsoon circulation than to the LLS CEFs. The East Asian summer monsoon circulation anomalies related to stronger LLA CEFs were associ- ated with less water vapor content and less rainfall in the region between the middle Yellow River and Yangtze River and with more water vapor and more rainfall in southern China. The sea-surface tempera- ture anomalies east of Australia related to summer LLA CEFs emerge in spring and persist into summer, with implications for the seasonal prediction of summer rainfall in East Asia. The connection between the LLA CEFs and East Asian summer monsoon rainfall may be partly due to its linkage with E1 Nino-Southern Oscillation. In addition, both the LLA and LLS CEFs .exhibited interdecadal shifts in the late 1970s and the late 1990s, consistent with the phase shifts of Pacific Decadal Oscillation （PDO）.

关键词： cross-equatorial flow Asian summer monsoon low-level jet Somali

基于IPCC AR4耦合模式的南极涛动和北极涛动的模拟及未来变化预估

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气象学报 2008年第6期66卷 993-1004页

作者：祝亚丽王会军中国科学院大气物理研究所北京100029 中国科学院研究生院北京100049

评估了参加政府间气候变化委员会第4次评估报告(IPCCAR4)的耦合模式对南极涛动和北极涛动的模拟能力。分析了24个模式对1970—1999年南极涛动和北极涛动的模拟效能,并与两套再分析资料ERA-40和NCEP-1进行了对比分析。结果表明,模式的模... 详细信息

评估了参加政府间气候变化委员会第4次评估报告(IPCCAR4)的耦合模式对南极涛动和北极涛动的模拟能力。分析了24个模式对1970—1999年南极涛动和北极涛动的模拟效能,并与两套再分析资料ERA-40和NCEP-1进行了对比分析。结果表明,模式的模拟能力具有一定的季节依赖性,冬季模拟能力最好。大多数模式对南极涛动空间结构和时间序列趋势的模拟好于北极涛动。根据Taylor图选出具有较好模拟能力的模式并做集合分析,发现经过选取的模式集合可以明显改善模式的模拟能力。分析SRESA1B情景下的南极涛动和北极涛动的模拟、预估结果表明:1970—2099年,南极涛动和北极涛动指数均呈持续上升趋势,北极涛动指数增长略显平稳。相对于1970—1999年、2060—2089年两半球的海平面气压场均呈现极区气压降低、中纬度气压升高的形态,同样表明南、北极涛动在后一时段更强。因此,在气候变暖背景下,南、北极涛动将持续增强,21世纪中期的臭氧恢复可能不会显著影响这种趋势。

关键词：南极涛动北极涛动 IPCC 耦合模式环状模

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近50年黄河流域气温变化特征及背景分析

气候与环境研究 2014年第4期19卷 477-485页

作者：潘攀祝亚丽王纪军河南省气候中心郑州450003 中国科学院大气物理研究所竺可桢-南森国际研究中心北京100029

利用1961-2010年黄河流域142个气象观测站的资料，详细分析了近50年黄河流域气温的时空分布和变化特征。黄河流域四季平均气温均呈现东部高、西部低、南部高、北部低的空间型态。对流域气温进行经验正交分解，第一模态呈现全流域一致的... 详细信息

利用1961-2010年黄河流域142个气象观测站的资料，详细分析了近50年黄河流域气温的时空分布和变化特征。黄河流域四季平均气温均呈现东部高、西部低、南部高、北部低的空间型态。对流域气温进行经验正交分解，第一模态呈现全流域一致的增温形势，上游增温幅度最大[0．40℃（10a）^-1]；第二模态表现为东西部反相变化；第三模态为南北部反相变化。四季气温随时间变化均呈现上升趋势，升温幅度冬季最大[0．52℃（10a）^-1]，其次是春季[0．30℃（10a）^-1]、秋季[0．26℃（10a）^-1]、夏季[0．14℃（10a）^-1]。进一步分析表明，近50年来，黄河流域的气温增暖除了全球变暖的影响，可能还来自1980年代中期和1990年代后期两次年代际增暖的贡献，这与东亚季风的两次年代际变化时间节点是一致的。

关键词：黄河流域气温气候变化年代际变化

The Recent Interdecadal and Interannual Variation of Water Vapor Transport over Eastern China

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Advances in Atmospheric Sciences 2011年第5期28卷 1039-1048页

作者：孙博祝亚丽王会军 Nansen-Zhu International Research Centre Institute of Atmospheric PhysicsChinese Academy of Sciences Beijing 100029 College of Earth Science Graduate University of Chinese Academy of Sciences Beijing 100049 College of Atmospheric Sciences Lanzhou University Lanzhou 7300004 Climate Change Research Centre Chinese Academy of Sciences Beijing 100029

The climatological characteristics and interdecadal variability of the water vapor transport and budget over the Yellow River-Huaihe River valleys （YH1） and the Yangtze River-Huaihe River valleys （YH2） of East China were investigated in this study,using the NCEP/NCAR monthly mean reanalysis datasets from 1979 to *** in the water vapor transport pattern occurred during the late 1990s over YH1 （YH2） that corresponded with the recent interdecadal changes in the eastern China summer precipitation *** net moisture influx in the YH1 increased and the net moisture influx in the YH2 decreased during 2000-2009 in comparison to *** features in the moisture flux and transport changes across the four boundaries were *** altered water vapor transport over the two domains can be principally attributed to the additive effects of the changes in the confluent southwesterly moisture flow by the Indian summer monsoon and East Asian summer monsoon （related with the eastward recession of the western Pacific subtropical high）.The altered water vapor transport over YH1 was also partly caused by the weakened midlatitude westerlies.

关键词： water vapor transport interdecadal variability summer monsoon midlatitude westerlies

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给你起一个爱的昵称

班主任之友(小学版) 2020年第5期 58-59页

作者：祝亚丽天津华夏未来中新生态城小学

序:想好了题目,却盯着电脑半天不知怎样开头。说实话,作为一位语文老师,今年已是我从教的第三个年头,但我对自己的定位还只是一个业界小白。从来没有写过任何文章,更不用说发表文章。我总会给自己找些借口,觉得自己文采不好,写不出来,...

序:想好了题目,却盯着电脑半天不知怎样开头。说实话,作为一位语文老师,今年已是我从教的第三个年头,但我对自己的定位还只是一个业界小白。从来没有写过任何文章,更不用说发表文章。我总会给自己找些借口,觉得自己文采不好,写不出来,或者工作太忙,没有时间静下来思考。但这次我想写点什么东西,起因于《班主任之友》这本杂志。

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The Relationship between the Aleutian Low and the Australian Summer Monsoon at Interannual Time Scales

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Advances in Atmospheric Sciences 2010年第1期27卷 177-184页

作者：祝亚丽王会军 Nansen-Zhu International Research Center Institute of Atmospheric PhysicsChinese Academy of Sciences Graduate University of Chinese Academy of Sciences Climate Change Research Center(CCRC) Chinese Academy of Sciences

The relationship between the boreal winter （December, January, February） Aleutian Low （AL） and the simultaneous Australian summer monsoon （ASM） is explored in this study. A significant correlation is found between the North Pacific index （NPI） and ASM index, the bulk of which is attributed to the significant correlation after late 1970s. Significant differences in precipitation and outgoing long-wave radiation between typical negative and positive NPI years appear over the ASM area. A regression analysis of the circulation pattern against the NPI during the three months is performed separately. We propose that the NPI is related with the ASM circulation possibly through the changes in the upper level westerly jet. In a typical negative NPI （strong Aleutian Low） year, the jet is greatly reinforced and the anomalous anticyclonic circulation to the south is thus excited, from which the easterly wind anomalies flowing into the ASM region emanate. Further, strong sinking motion over the northern entrance region of the jet is enhanced, and the local Hadley circulation anomaly between the ASM region and the coast of East Asia is strengthened. In this way, anomalous upward motion over the ASM area can thus be strengthened, and the convective activity intensified. Then the monsoon rainfall over ASM area is increased. An ＂asymmetric＂ connection between AL and the monsoon is found in this study.

关键词： North Pacific Aleutian Low Australian monsoon interannual variability

The Arctic and Antarctic Oscillations in the IPCC AR4 Coupled Models

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Acta meteorologica Sinica 2010年第2期24卷 176-188页

作者：祝亚丽王会军 Nansen-Zhu International Research Center Institute of Atmospheric PhysicsChinese Acadamy of Sciences Graduate School of Chinese Academy of Sciences Climate Change Research Centre Chinese Academy of Sciences

This study evaluates the fidelity of Arctic and Antarctic oscillations（AO and AAO for short,respectively） in the coupled general circulation models participating in the Fourth Assessment Report of Intergovernmental Panel on Climate Change（IPCC AR4）.The AO and AAO during 1970-1999 in 24 models are analyzed and compared with that in ERA-40 and ***＇ performance is seasonally dependent,with best reproducibility of both spatial structure and trend in *** most models,the spatial pattern and temporal trend of AAO during this period are more delicately simulated than *** picking out models with better performance according to the Taylor diagram,we find that their ensemble mean can obviously improve models＇ *** AO and AAO in the Special Report on Emission Scenarios（SRES） A1B Projection during the 21st century are also briefly *** results reveal that both the AO and AAO indices keep increasing during 1970-2099,with a steadier pace of AO than *** spatial difference of sea level pressure between 2060-2089 and 1970-1999 shows decreased values in polar regions,and increased values in *** results manifest that the ozone recovery during the mid 21st century may not weaken such a trend.

关键词： Antarctic oscillation Arctic oscillation IPCC coupled model annular mode