An Incursion of Off-Equatorial Subsurface Cold Water and Its Role in Triggering the “Double Dip” La Nia Event of 2011

Based on Global Ocean Data Assimilation System(GODAS) and NCEP reanalysis data, atmospheric and oceanic processes possibly responsible for the onset of the 2011/12 La Nia event, which followed the 2010/11 La Nia even—referred to as a "double dip" La Nia—are investigated. The key mechanisms involved in activating the 2011/12 La Nia are illustrated by these datasets. Results show that neutral conditions were already evident in the equatorial eastern Pacific during the decaying phase of the 2010/11 La Nia. However, isothermal analyses show obviously cold water still persisting at the surface and at subsurface depths in off-equatorial regions throughout early 2011, being most pronounced in the tropical South Pacific. The negative SST anomalies in the tropical South Pacific acted to strengthen a southern wind across the equator. The subsurface cold water in the tropical South Pacific then spread northward and broke into the equatorial region at the thermocline depth. This incursion process of off-equatorial subsurface cold water successfully interrupted the eastern propagation of warm water along the equator, which had previously accumulated at subsurface depths in the warm pool during the 2010/11 La Nia event. Furthermore, the incursion process strengthened as a result of the off-equatorial effects, mostly in the tropical South Pacific. The negative SST anomalies then reappeared in the central basin in summer 2011, and acted to trigger local coupled air–sea interactions to produce atmospheric–oceanic anomalies that developed and evolved with the second cooling in the fall of 2011.     

中祁连西段野马山岩基年代学、地球化学特征及地质意义

野马山岩基位于中祁连地块西段,由早期岩体(花岗闪长岩、斑状二长花岗岩)和晚期岩体(二长花岗岩)组成,二者呈侵入接触。LA-ICPMS锆石U-Pb定年表明,早期岩体侵位时代为中奥陶世((469.0±1.3)Ma),晚期岩体侵位时代为晚奥陶世((450.0±1.0)Ma)。早期岩体Si O2=59.8%~64.2%,K2O/Na2O1,且A/NKC=0.8~1.0,为准铝质岩石;微量元素相对富集Rb、U、Th和亏损Ba、Nb、Ta、Sr、P、Ti;稀土总量为97.7×10-6~185×10-6,且(La/Yb)N=5.57~12.47,LREE/HREE=7.7~11.3,具轻重稀土分馏明显,轻稀土富集,弱Eu负异常(δEu=0.66~0.89)特征。晚期岩体Si O2=69.8%~76.5%、K2O/Na2O=1.2~1.7、A/NKC=1.0~1.1,属弱过铝质花岗岩;稀土总量为78.97×10-6~244.92×10-6,轻重稀土分馏不明显((La/Yb)N=1.90~5.72),强Eu负异常(δEu=0.11~0.24)。岩石地球化学特征表明,野马山岩基早期岩体为I型花岗岩,形成于俯冲环境,晚期岩体为高分异的I型花岗岩,形成于后碰撞环境。结合岩体产出的区域构造位置及区域地质演化,认为早古生代北祁连洋发生了双向俯冲,野马山岩基为其向南俯冲碰撞的产物。     

实时路况支持下的南京市消防救援覆盖率时空模式分析

快速城镇化导致我国城市消防应急服务基础设施与城市发展不同步的问题日益凸显,城市消防救援覆盖率评估是提升消防服务质量与优化消防资源配置的重要手段。本文提出一种基于实时路况的城市消防救援覆盖率评估模型,通过考虑消防站管辖区域的空间限制,在2020年9月连续三周时间内利用高德地图API获取消防站到达历史火灾事件的实时出行救援时间,对南京市消防救援覆盖率的时空模式进行分析与挖掘。结果显示：① 南京城市火灾密集区域（简称火灾密集区）消防站的平均出行救援时间约10 min,非火灾密集区约16 min,均比国家规定的5 min到达时间标准明显要长,导致南京市消防站在5 min到达标准下的覆盖率仅为8.2%;② 由于南京火灾密集区消防站的平均行车救援距离仅为非火灾密集区的37%,导致火灾密集区火灾事件等待救援时间明显低于非火灾密集区,尤其火灾密集区西南部、东北部及部分消防站周边火灾事件等待救援时间相对较短,但南京全区火灾事件等待救援时间在5 min以内的比例不足7%,且等待救援时间在5~10 min之间的短距离火灾事件受早晚交通出行高峰期交通拥堵影响最大;③ 南京市消防站救援覆盖率受早晚交通出行高峰影响呈现早晚交通出行高峰期明显低于其他时段的“W”形变化模式,火灾密集区消防站在5 min到达标准下的救援覆盖率从非交通出行高峰期的11.5%降低到交通出行高峰期的8.4%,而非火灾密集区从6.1%降低到5%,火灾密集区东南部石门坎与东山交界区域和北部汉中门与迈皋桥周边区域早晚交通出行高峰时段等待救援时间超过15 min的火灾事件比非交通出行高峰时段明显增多;④ 在5 min到达标准下,南京市消防站救援覆盖率“W”形模式波动最小,10 min到达标准下的平均覆盖率为43.5%且波动最明显,15 min到达标准下的平均覆盖率达到75%。最后根据分析结果给出了南京市消防未来建设发展意见。     

基于高分卫星影像的复杂山区光伏电站信息提取

该文基于高分卫星资料,通过基于规则的面向对象分类、基于最邻近法的监督分类及基于CART分类器的监督分类三种不同分类方法,对复杂山区光伏电站进行提取,对比三种分类提取方法结果并完成精度验证。结果表明,合理的分割参数有利于提高光伏电站提取精度;基于规则的面向对象分类法光伏电站提取精度最佳,最邻近分类法次之,CART分类器分类法最差,可利用基于规则的面向对象分类法较为准确地进行复杂山区光伏电站信息提取,为光伏产业健康、合理发展提供一定的数据支撑。     

Mesozoic–Cenozoic multistage tectonic evolution of the Pamir: Detrital fission-track constraints from the Tajik Basin

Knowledge of the tectonic history of the Pamir contributes to our understanding of both the evolution of collisional orogenic belts as well as factors controlling Central Asian aridification. It is, however, not easy to decipher the Mesozoic–Cenozoic tectonics of the Pamir due to extensive Neogene deformation in an orogen that remains largely understudied. This study reports detrital apatite and zircon fission-track (FT) ages from both the eastern Tajik Basin sedimentary rocks and Pamir modern river sands. These FT data, supported by vitrinite reflectance and zircon and apatite U–Pb double dating, suggest that the majority of the FT ages are unreset and record exhumation stages of the Pamir, which has served as the source terrane of the Tajik Basin since the Cretaceous. Furthermore, we combine the new data with a compilation of published detrital apatite and zircon FT data from both the Tajik Basin sedimentary rocks and Pamir modern river sands, to explore the Mesozoic–Cenozoic tectonic history of Pamir. Deconvolved FT Peak Ages document two major Mesozoic exhumation events associated with the Late Triassic–Early Jurassic Cimmerian orogeny that reflects accretion of the Pamir terranes, as well as the Early–early Late Cretaceous deformation associated with the northward subduction of the Neo-Tethys Ocean beneath Pamir. The compiled data also show significant Late Eocene–Neogene exhumation associated with the ongoing formation of the Pamir, which peaks at ca. 36, 25, 14 and 7 Ma.     

南极长城站能见度变化分析

利用南极长城站1986—2012年能见度人工观测资料,分析了能见度的变化特征和趋势。结果显示,高于10 km能见度出现频率为61.0%,低于1 km的频率为8.0%。11—3月能见度较好,6—10月能见度较差;海雾和降水是夏季能见度降低的主要原因,冬季则主要归因于频繁的降雪、吹雪或雪暴等灾害性天气。10 km能见度发生频数有显著减小倾向,10 km能见度呈上升趋势,且冬季的上升速度最快,大雾、吹雪和降雪减少是主导冬季能见度升高趋势的重要因素。长城站能见度显著的天气尺度周期为2.1—8.3 d,年际变化周期为2 a、4.1 a和6.9—8.2 a,又以4.1 a最为显著。2012年开展的能见度自动观测实验表明,20 km范围内的自动观测精度较高,适用于长城站的连续监测。     

台站迁移对甘肃省气温记录均一性影响的检验

针对气象台站气温观测资料序列存在站址迁移可能造成的资料非均一性影响,利用环县等6个站址迁移气象站的逐年平均气温、平均最高气温、平均最低气温序列,采用SNHT(标准正态检验)客观分析方法,结合6个气象站的元数据及历史沿革资料等信息进行主观分析,对因迁站造成的气温序列不均一性进行检验,表明站址迁移对气温资料影响较大,并且因地理地形环境而有所差异。结果表明:台站迁移后造成新旧站址的地理环境差异显著且海拔高度差异过大,是引起气温序列非均一性的主要原因。地理环境、气候条件相似的台站迁移对气温资料的均一性无明显影响。     

WUSH-TV2型超声蒸发传感器的安装与维护

介绍WUSH-TV2型超声蒸发传感器的系统组成、工作原理以及安装方法,并对实际工作运行中遇到的故障进行分析,提出了合理的保障维护方法和处理思路.     

临河气象观测站迁移对气象要素的影响分析

文章通过对内蒙古巴彦淖尔市临河地面气象观测站迁移前、后4a的自动气象站观测要素对比分析,得出临河迁站前、后气象要素存在明显的差异:新站的年、月平均气温比旧站低、相对湿度比旧站高、风速比旧站大。旧站的观测资料仅代表城市中心局部气候状况,已经不能较好的反映本地区的气候特点;而新站则较好的反映了临河地区城郊大范围的天气气候状况。同时分析了新、旧站各气象要素差值的形成原因,期望为天气预报、气候评价、气象服务等提供数据参考。