The leading correlation of the winter Aleutian Low with surface air temperature during the subsequent summer over the Arctic and its possible mechanism

The variations of surface air temperature(SAT)over the Arctic are closely related to global climate change.Based on reanalysis datasets and a newly defined Aleutian Low intensity index,we found a good correlation between intensity of winter Aleutian Low and the SAT over the Arctic during the subsequent summer.Explanations were given using correlation analysis,composite analysis,and singular value decomposition methods.When intensity of winter Aleutian Low was weaker,sea surface temperature appeared higher in the North Pacific in the subsequent spring and summer,resulting in mean meridional circulation anomalies and 500 hPa geopotential height anomalies in spring and summer.Anomalous upward motion in mid-latitudes and downward motion in high latitudes(Ferrel cell weakening)transported the warmer air to the north from lower layer to the upper layer followed by increases in the SAT over the Arctic.Anomalous downward motion over about 75°N also caused consequent adiabatic warming and contributed to inhibit the heat transportation from surface to upper layer.Negative 500 hPa geopotential height anomalies existed in mid-latitudes and positive anomalies existed in high latitudes.The pattern(low-in-south and high-in-north)benefited from increasing the inflow volume flux of the Bering Strait,which also made the SAT over the Arctic increase.The results of this study reveal the process that the summer SAT over the Arctic was modulated by interannual variability of intensity of winter Aleutian Low.     

Maxiconv8000型抑焦增液剂在延迟焦化装置的应用

为延长装置生产周期、提高液体收率、增加经济效益,中国石油大庆石化分公司延迟焦化装置使用了Maxiconv8000型抑焦增液剂。结果表明,在装置操作条件稳定,注剂量为70 /g时,焦炭和干气的产率分别降低0.39%和0.93%,轻质油收率和总液体收率分别增加了0.67%和1.32%;加热炉炉管表面温度大幅下降,加热炉炉管压降减小,有效地减缓了加热炉炉管结焦。     

厄尔尼诺与湖北暖冬及冷冬的关系

根据１９５１－１９９８年湖北１－２月气温资料,研究了湖北冬季温度变化同北 温的联系及相关结构,具体描术字在厄尔尼群诺年和拉尼娜年湖北冬季温度距平的差异性,结论是在厄尔尼诺年湖北冬季温度明显偏高,易出现暖冬,拉尼娜年则相反,易出现冷冬。     

摩擦系数对AMT起步的影响分析

根据摩擦因数随摩擦副表面温度的改变,研究了摩擦因数在电控机械自动变速汽车重复起步过程中的影响.建立了AMT起步时离合器传递转矩和压盘表面温升的模型.根据试验结果,采用“快-慢-快”起步控制策略,利用Matlab/Simulink进行汽车重复起步仿真,进行了摩擦副滑摩功仿真计算.仿真结果表明,摩擦系数随滑摩功的变化而变化,重复起步多次后,摩擦系数变得很小,相应离合器传递的转矩也变得很小,离合器主、从动盘一直处于滑磨状态,无法完成正常起步.     

Sea surface temperature and terrestrial biomarker records of the last 260 ka of core MD05-2904 from the northern South China Sea

This paper reports high-resolution biomarker records of the last 260 ka for core MD05-2904 from the northern South China Sea （SCS）. The sea surface temperature （SST） record using the U37^k＇, index reveals a minimum of 21.5℃（MIS 2） and a maximum of 28.3℃（MIS 5.5）, for a temperature difference of almost 7℃, and provides the longest high-resolution U37^k＇ SST record in northern SCS. The content of odd-number long chain n-alkanes and several n-alkanes indexes such as the CPI, ACL and the C31/C27 ratio, all reveal generally higher values during the glacials and lower values during the interglaclals. Terrestrial input as Indicated by n-alkane content was mostly controlled by sea-level changes： During the glacials, lower sea-level exposed the continental shelf to enable rivers to transport more terrestrial materials to the slope; and the situation reverses during the interglacials. The n-alkane indexes changes reveal more n-alkanes from contemporary vegetation during glacials as a result of the proximity of the core site to the source region, while the increases in ACL and C81/C27 ratio during glaclals indicate a change to more grassy vegetation. However, the highest values for CPI, ACL and the C81/C27 ratio all occurred during late MIS 3, and it was suggested that this period was characterized by a strong summer monsoon-dominated humid climate which resulted in a denser vegetation for the exposed continental shelf region.     

Comparison of summer thermohaline field and circulation structure of the Bohai Sea between 1958 and 2000

TheBohaiSea(37°07′—41°N,117°35′—121°10′E)isashallowsemi-enclosedsea.SincetheBohaiSeaistheonlyinnerseaofChinaandalsoanimportantstra-tegicsea,itisoneofthemostinvestigatedseasinChina.Alargenumberofstudiesonthetideandthetidalcurrentaswellasnumericalsimulationofcirculationhavebeencarriedout,enhancingourunderstandingoftheBohaiSea.Long-termvariationsoftheseasurfacesalinity(SSS)andseasurfacetemperature(SST)oftheBohaiSeawereanalyzed.Linetal.[1]foundthatthepositivetrendsoftheannualmeanS…     

利用ETM+和MODIS数据反演陆地表面温度

Landsat 7 ETM +数据是一种常用的中分辨率卫星遥感数据,它的热红外波段的空间分辨率为60 m,是目前星载遥感数据中分辨率最高的.然而由于Landsat 7 ETM +只有一个热红外波段,给ETM +陆地表面温度反演造成了困难.在前人研究的基础上开展ETM +数据陆地表面温度反演研究,首先利用MODIS数据反演总大气水蒸汽含量,然后利用普适性单通道算法从ETM +数据得到陆地表面温度,试验结果表明该方法能够取得较好的反演结果.     

科学家发现一比地球小的太阳系外行星

美国航天局7月18日宣布,天文学家利用该局的"斯皮策"太空望远镜发现一颗大小只有地球三分之二的太阳系外行星。这颗行星名为UCF-1.01,距地球约33光年,表面温度非常高,可能是与太阳系距离最近的小于地球的系外行星。相     

生物组织中异常热源信息获取方法

为通过相对简单的热传递模型建立表面温度分布与内部热源之间的关系,从生物传热理论出发,研究了内热源影响下的组织表面温度分布,实现了在表面温度分布已知的情况下得到内部热源的相关信息.基于傅里叶定律和能量守恒定律建立了具有内热源的组织导热微分方程,通过求解微分方程推导出组织表面温度分布与内部异常热源之间的组织传热模型,采用有限元分析方法对该模型进行模拟计算和数值分析.考虑了两种不同情况下的组织内部异常热源信息的获取,所得结果(1.64 cm、1.56 cm、1.55 cm和0.78 cm、1.64 cm、2.55 cm)与根据热断层成像技术估测所得的热源深度(1.6 cm和0.8 cm、1.6 cm、2.5 cm)十分接近,验证了模型的可行性与准确性.     

Changes in sea surface temperature in western South China Sea over the past 450 ka

Sea surface temperature over the past 450 ka was obtained by the unsaturation of molecular fossil-long chain alkenone with a resolution of about 1 ka from the western South China Sea. This is the longest temperature profile in the South China Sea at such high resolution. The U37^κ-SST results revealed similar glacial-interglacial cycles as the δ^18O profile of planktonic foraminifera, with SST variability of 23-25.5℃ for glacial and 25-28℃ for interglacial periods. The highest SST （28.4℃） was recorded at MIS5.5 and lowest SST （22.6℃） during MIS2. The SST record preceded the planktonic foraminiferal δ^18O on five glacial-interglacial transitions. Comparison of temperature records from the Southern and Northern Hemispheres indicated a more Southern Hemisphere-like pattern for the temperature variation in the SCS. Strong precession and semiprecession signals in the spectra of our SST record manifest the tropical phenomena.