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地方红色文化资源融入新疆开放大学课程建设的实践研究

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文化创新比较研究 2024年第4期8卷 137-142页

作者：宋雅娟阚利萍魏永涛吐鲁番职业技术学院新疆吐鲁番838000 南京工业大学经济与管理学院江苏南京211816

中国式现代化离不开大学的配合与支持,高质量、高效和富有地方特色的校园课程文化建设是当前和未来背景下多民族地区文化创新的必由之路。该文研究内容包括地方红色文化资源及其文献发展情况、红色文化资源融入课程建设意义与实践等,研... 详细信息

中国式现代化离不开大学的配合与支持,高质量、高效和富有地方特色的校园课程文化建设是当前和未来背景下多民族地区文化创新的必由之路。该文研究内容包括地方红色文化资源及其文献发展情况、红色文化资源融入课程建设意义与实践等,研究方法为文献研究、案例研究和实证分析等,发现在大学校园课程文化建设过程中,发挥当地丰富红色文化资源的价值,实现文化教育的当代功能是必要的。该文旨在提高学生的民族自豪感和文化认同感,激发他们对于历史使命的责任意识和爱国情怀,培养他们的奋斗精神、奉献意识,使得大学校园课程文化建设更具吸引力、活力和影响力。

关键词：红色文化文化资源新疆开放大学课程建设实践文化教育研究意义

FIO-ESM v2.0 CORE2-forced experiment for the CMIP6 Ocean Model Intercomparison Project

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Acta Oceanologica Sinica 2022年第10期41卷 22-31页

作者： Qi Shu Zhenya song Ying Bao Xiaodan Yang yajuan song Xinfang Li Meng Wei Fangli Qiao First Institute of Oceanography and Key Laboratory of Marine Science and Numerical ModelingMinistry of Natural ResourcesQingdao266061China Laboratory for Regional Oceanography and Numerical Modeling Pilot National Laboratory for Marine Science and Technology(Qingdao)Qingdao266237China Shandong Key Laboratory of Marine Science and Numerical Modeling Qingdao266061China

We introduced the Coupled Model Intercomparison Project Phase 6(CMIP6)Ocean Model Intercomparison Project CORE2-forced(OMIP-1)experiment by using the First Institute of Oceanography Earth System Model version 2.0(FIO-ESM v2.0),and comprehensively evaluated the simulation *** other OMIP models,FIO-ESM v2.0 includes a coupled ocean surface wave component model that takes into account non-breaking surface wave-induced vertical mixing in the ocean and effect of surface wave Stokes drift on air-sea momentum and heat fluxes in the climate system.A sub-layer sea surface temperature(SST)diurnal cycle parameterization was also employed to take into account effect of SST diurnal cycle on air-sea heat fluxes to improve simulations of air-sea *** show that mean values and long-term trends of significant wave height were adequately reproduced in the FIO-ESM v2.0 OMIP-1 simulations,and there is a reasonable fit between the SST diurnal cycle obtained from in situ observations and that parameterized by FIO-ESM *** of model drift,temperature,salinity,mixed layer depth,and the Atlantic Meridional Overturning Circulation show that the model performs well in the FIO-ESM v2.0 OMIP-1 ***,the summer sea ice extent of the Arctic and Antarctic is underestimated.

关键词： FIO-ESM OMIP CMIP6 OGCM

QuEChERS-HPLC-MS/MS法同时测定韭菜中18种杀菌剂残留

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食品工业 2024年第2期45卷 302-305页

作者：单平阳宋亚娟黄月王磊石可歆董浩爽唐山市食品药品综合检验检测中心唐山063000 河北省农产品质量安全检测技术创新中心唐山063000 唐山市功能性农产品产业技术研究院唐山063000

以韭菜为试验原料,利用QuEChERS法对韭菜样品进行净化,建立高效液相色谱-串联质谱法(HPLCMS/MS)同时测定韭菜中18种杀菌剂残留量的方法。结果表明,选用Phenomenex双苯基色谱柱分离,18种杀菌剂的保留时间在2.8~8.0 min之间。质量浓度范围... 详细信息

以韭菜为试验原料,利用QuEChERS法对韭菜样品进行净化,建立高效液相色谱-串联质谱法(HPLCMS/MS)同时测定韭菜中18种杀菌剂残留量的方法。结果表明,选用Phenomenex双苯基色谱柱分离,18种杀菌剂的保留时间在2.8~8.0 min之间。质量浓度范围在0.01~0.08μg/mL时,各种杀菌剂的线性关系良好,相关系数(r)均≥0.9990,方法检出限(r_(SN)=3)为0.11~0.87μg/kg,定量限0.65~1.89μg/kg,在5.0,10.0和50.0μg/kg这3个质量分数水平上加标平均回收率为87%~108%,相对标准偏差(n=6)为2.1%~4.5%。该方法操作简单、灵敏准确,可用于韭菜中18种杀菌剂的残留量测定。

关键词： HPLC-MS/MS QuEChERS 韭菜杀菌剂

Link between the Barents Oscillation and Recent Boreal Winter Cooling over the Asian Midlatitudes

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Advances in Atmospheric Sciences 2018年第1期35卷 127-132页

作者： Qi SHU Fangli QIAO Zhenya song yajuan song First Institute of Oceanography State Oceanic Administration Laboratory for Regional Oceanography and Numerical Modeling Qingdao National Laboratory for Marine Science and Technology Key Laboratory of Marine Science and Numerical Modeling State Oceanic Administration

The link between boreal winter cooling over the midlatitudes of Asia and the Barents Oscillation(BO) since the late 1980s is discussed in this study, based on five datasets. Results indicate that there is a large-scale boreal winter cooling during 1990–2015 over the Asian midlatitudes, and that it is a part of the decadal oscillations of long-term surface air temperature(SAT)anomalies. The SAT anomalies over the Asian midlatitudes are significantly correlated with the BO in boreal winter. When the BO is in its positive phase, anomalously high sea level pressure over the Barents region, with a clockwise wind anomaly,causes cold air from the high latitudes to move over the midlatitudes of Asia, resulting in anomalous cold conditions in that region. Therefore, the recent increasing trend of the BO has contributed to recent winter cooling over the Asian midlatitudes.

关键词： climate change Barents Oscillation winter cooling

Tropical Cyclone Genesis Potential Index over the Western North Pacific Simulated by CMIP5 Models

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Advances in Atmospheric Sciences 2015年第11期32卷 1539-1550页

作者： song yajuan WANG Lei LEI Xiaoyan WANG Xidong College of Physical and Environmental Oceanography Ocean University of China First Institute of Oceanography State Oceanic Administration State Key Laboratory of Tropical Oceanography South China Sea Institute of OceanologyChinese Academy of Sciences Key Laboratory of Marine Environment Information Technology State Oceanic Administration

Tropical cyclone （TC） genesis over the western North Pacific （WNP） is analyzed using 23 CMIP5 （Coupled Model Intercomparison Project Phase 5） models and reanalysis datasets. The models are evaluated according to TC genesis potential index （GPI）. The spatial and temporal variations of the GPI are first calculated using three atmospheric reanalysis datasets （ERA-Interim, NCEP/NCAR Reanalysis- 1, and NCEP/DOE Reanalysis-2）. Spatial distributions of July-October-mean TC frequency based on the GPI from ERA-interim are more consistent with observed ones derived from IBTrACS global TC data. So, the ERA-interim reanalysis dataset is used to examine the CMIP5 models in terms of reproducing GPI during the period 1982-2005. Although most models possess deficiencies in reproducing the spatial distribution of the GPI, their multi- model ensemble （MME） mean shows a reasonable climatological GPI pattern characterized by a high GPI zone along 20°N in the WNP. There was an upward trend of TC genesis frequency during 1982 to 1998, followed by a downward trend. Both MME results and reanalysis data can represent a robust increasing trend during 1982-1998, but the models cannot simulate the downward trend after 2000. Analysis based on future projection experiments shows that the GPI exhibits no significant change in the first half of the 21st century, and then starts to decrease at the end of the 21st century under the representative concentration pathway （RCP） 2.6 scenario. Under the RCP8.5 scenario, the GPI shows an increasing trend in the vicinity of 20°N, indicating more TCs could possibly be expected over the WNP under future global warming.

关键词： tropical cyclone genesis potential index CMIP5 western North Pacific global warming.

Seasonal prediction skills of FIO-ESM for North Pacific sea surface temperature and precipitation

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Acta Oceanologica Sinica 2019年第1期38卷 5-12页

作者： Yiding Zhao Xunqiang Yin yajuan song Fangli Qiao College of Oceanic and Atmospheric Sciences Ocean University of China First Institute of Oceanography Ministry of Natural Resources Laboratory for Regional Oceanography and Numerical Modeling Pilot National Laboratory for Marine Science and Technology (Qingdao) Key Laboratory of Marine Science and Numerical Modeling Ministry of Natural Resources

The seasonal prediction of sea surface temperature(SST) and precipitation in the North Pacific based on the hindcast results of The First Institute of Oceanography Earth System Model(FIO-ESM) is assessed in this *** Ensemble Adjusted Kalman Filter assimilation scheme is used to generate initial conditions, which are shown to be reliable by comparison with the observations. Based on this comparison, we analyze the FIO-ESM 6-month hindcast results starting from each month of 1993–2013. The model exhibits high SST prediction skills over most of the North Pacific for two seasons in advance. Furthermore, it remains skillful at long lead times for midlatitudes. The reliable prediction of SST can transfer fairly well to precipitation prediction via air-sea *** average skill of the North Pacific variability(NPV) index from 1 to 6 months lead is as high as 0.72(0.55) when El Ni?o-Southern Oscillation and NPV are in phase(out of phase) at initial conditions. The prediction skill of the NPV index of FIO-ESM is improved by 11.6%(23.6%) over the Climate Forecast System, Version 2. For seasonal dependence, the skill of FIO-ESM is higher than the skill of persistence prediction in the later period of prediction.

关键词： seasonal prediction North Pacific sea surface temperature precipitation FIO-ESM climate model

Could CMIP6 climate models reproduce the early-2000s global warming slowdown?

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Science China Earth Sciences 2021年第6期64卷 853-865页

作者： Meng WEI Qi SHU Zhenya song yajuan song Xiaodan YANG Yongqing GUO Xinfang LI Fangli QIAO First Institute of Oceanography and Key Laboratory of Marine Science and Numerical ModelingMinistry of Natural ResourcesQingdao266061China Laboratory for Regional Oceanography and Numerical Modeling Pilot National Laboratory for Marine Science and TechnologyQingdao266237China Shandong Key Laboratory of Marine Science and Numerical Modeling Qingdao266061China Marine Science and Technology College Zhejiang Ocean UniversityZhoushan316000China

The unexpected global warming slowdown during 1998–2013 challenges the existing scientific understanding of global temperature change mechanisms,and thus the simulation and prediction ability of state-of-the-art climate models since most models participating in phase 5 of the Coupled Model Intercomparison Project(CMIP5)cannot simulate ***,we examine whether the new-generation climate models in CMIP6 can reproduce the recent global warming slowdown,and further evaluate their capacities for simulating key-scale natural variabilities which are the most likely causes of the *** results show that although the CMIP6 models present some encouraging improvements when compared with CMIP5,most of them still fail to reproduce the warming *** considerably overestimate the warming rate observed in 1998–2013,exhibiting an obvious warming acceleration rather than the observed *** is probably associated with their deficiencies in simulating the distinct temperature change signals from the human-induced long-term warming trend and/or the three crucial natural variabilities at interannual,interdecadal,and multidecadal *** contrast,the 4 models that can successfully reproduce the slowdown show relatively high skills in simulating the long-term warming trend and the three keyscale natural *** work may provide important insight for the simulation and prediction of near-term climate changes.

关键词： CMIP6 climate models Global warming Global warming slowdown Hiatus Climate natural variability Anthropogenic warming trend

FIO-ESM v2.0 Outputs for the CMIP6 Global Monsoons Model Intercomparison Project Experiments

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Advances in Atmospheric Sciences 2020年第10期37卷 1045-1056页

作者： yajuan song Xinfang LI Ying BAO Zhenya song Meng WEI Qi SHU and Xiaodan YANG First Institute of Oceanography Ministry of Natural ResourcesQingdao 266061China Laboratory for Regional Oceanography and Numerical Modeling Qingdao National Pilot National Laboratory for Marine Science and TechnologyQingdao 266000China Key Laboratory of Marine Science and Numerical Modeling Ministry of Natural ResourcesQingdao 266061China

Three tiers of experiments in the Global Monsoons Model Intercomparison Project(GMMIP),one of the endorsed model intercomparison projects of phase 6 of the Coupled Model Intercomparison Project(CMIP6),are implemented by the First Institute of Oceanography Earth System Model version 2(FIO-ESM v2.0),following the GMMIP *** of global mean surface air temperature from 1870 to 2014 and climatological precipitation(1979–2014)in tier-1 shows that the atmosphere model of FIO-ESM v2.0 can reproduce the basic observed atmospheric *** tier-2,the internal variability is captured by the coupled model,with the SST restoring to the model climatology plus the observed anomalies in the tropical Pacific and North *** of the Northern Hemisphere summer monsoon circulation is significantly improved by the SST restoration in the North *** tier-3,five orographic perturbation experiments are conducted covering the period 1979–2014 by modifying the surface elevation or vertical heating in the prescribed *** particular,the strength of the South Asian summer monsoon is reduced by removing the topography or thermal forcing above 500 m over the Asian *** and daily simulated outputs of FIO-ESM v2.0 are provided through the Earth System Grid Federation(ESGF)node to contribute to a better understanding of the global monsoon system.

关键词： CMIP6 GMMIP FIO-ESM v2.0 global monsoon

Causes for different spatial distributions of minimum Arctic sea-ice extent in 2007 and 2012

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Acta Oceanologica Sinica 2015年第9期34卷 94-101页

作者： CUI Hongyan QIAO Fangli SHU Qi song yajuan JIANG Chunfei College of Physical and Environmental Oceanography Ocean University of China The First Institute of Oceanography State Oceanic Administration Key Laboratory of Marine Science and Numerical Modeling State Oceanic Administration

Satellite records show the minimum Arctic sea ice extents （SIEs） were observed in the Septembers of 2007 and 2012, but the spatial distributions of sea ice concentration reduction in these two years were quite different. Atmospheric circulation pattern and the upper-ocean state in summer were investigated to explain the difference. By employing the ice-temperature and ice-specific humidity （SH） positive feedbacks in the Arctic Ocean, this paper shows that in 2007 and 2012 the higher surface air temperature （SAT） and sea level pressure （SLP） accompanied by more surface SH and higher sea surface temperature （SST）, as a consequence, the strengthened poleward wind was favorable for melting summer Arctic sea ice in different regions in these two years. SAT was the dominant factor influencing the distribution of Arctic sea ice melting. The correlation coefficient is -0.84 between SAT anomalies in summer and the Arctic SIE anomalies in autumn. The increase SAT in different regions in the summers of 2007 and 2012 corresponded to a quicker melting of sea ice in the Arctic. The SLP and related wind were promoting factors connected with SAT. Strengthening poleward winds brought warm moist air to the Arctic and accelerated the melting of sea ice in different regions in the summers of 2007 and 2012. Associated with the rising air temperature, the higher surface SH and SST also played a positive role in reducing summer Arctic sea ice in different regions in these two years, which form two positive feedbacks mechanism.

关键词： Arctic sea ice extent atmospheric circulation upper-ocean feedback