2022年夏季中国高温的环流异常特征

基于美国国家海洋和大气管理局(National Oceanic and Atmospheric Administration, NOAA)全球范围扩展重建海面温度资料第5版本(Extended Reconstructed Sea Surface Temperature version 5,ERSSTv5),以及美国国家环境预报中心和国家大气研究中心NCEP(National Centers for Environmental Prediction)/NCAR(National Center for Atmospheric Research)逐月全球再分析资料,采用相关、回归、合成及物理量诊断等方法,对2022年夏季中国大范围高温相关环流异常的可能成因进行了分析。结果表明:(1)2022年夏季南亚高压偏强并分别向东、西方向扩展,西太平洋副热带高压(以下简称“副高”)异常偏强西伸。2022夏季为拉尼娜(La Nina)年,但热带大西洋垂直上升环流相对西太平洋更强,且热带印度洋到西太平洋热带垂直上升环流异常也偏强。(2)2022年热带大西洋、印度洋到西太平洋上空垂直环流异常和La Nina共同作用,使得夏季南亚高压和西太平洋副高极端异常。La Nina和印度洋到西太平洋垂直环流异常有利于南亚高压和西太平洋副高的偏强西伸;热带大西洋环流异常则既有利于南亚高压的加强及东扩,也有利于西太平洋副高偏强西伸。(3)印度洋到西太平洋垂直环流主要通过局地经向哈得来(Hadley)环流影响青藏高原到中国东部的环流异常,表现为青藏高原到中国东部中低层为显著的辐散异常;热带大西洋则通过引起纬向风异常(急流异常),激发遥相关波列并向下游传播,进而影响青藏高原到中国东部地区的环流异常。

合成平均图分析在2003年高温天气预报中的应用

大气环流异常对中短期天气变化有着重要影响。利用数值预报产品制作特征要素的合成平均图,是准定量分析前期大气环流异常对中短期天气变化造成影响的有效途径之一,也是对数值预报产品进行合理有效解释应用的一个重要方向。通过利用欧洲中心格点资料制作预报和历史同期合成平均图,结合本地经验指标进行分析比较,并根据临近天气形势进行中短期预报订正,是2003年广西持续性大范围高温天气过程成功预报的关键。

华中区域夏季日用电量气象预报模型研究

利用华中地区三省2004年～2006年夏季(6～8月)逐日用电量和气温资料,计算分析了湖北省及华中地区三省日用电量与对应区域日平均气温≥30℃的台站数、日平均气温、日最高气温和日最低气温的相关关系,并以前两年对应资料建立了用电量气象预报模型,以2006年的资料进行预报效果的独立样本检验。结果表明:日平均气温≥30℃的台站数与日用电量有较好的峰谷对应关系;日用电量与4个气象要素指标的相关性均达到极显著程度,其中又以与日平均气温的相关系数最高;应用逐步回归方法分别建立了湖北省及华中地区三省夏季日用电量气象预报模型,其中日平均气温≥30℃台站数均入选了预报方程;两套模型的预报值与实际值拟合效果都较好。

Properties of failure mode and thermal damage for limestone at high temperature

The mechanical properties of limestone such as the stress-strain curve, the variable characteristics of peak strength and the modulus of elasticity of limestone were studied under the action of temperatures ranging from room temperature to 800 °C.Our results show that:1) the temperature has not clear effect on the mechanical properties of limestone from room temperature to 600 °C.However, the mechanical properties of limestone deteriorate rapidly when the temperature is above 600 °C.In this case, the peak stress and modulus of elasticity decrease rapidly.When the temperature reaches 800 °C, the entire process, showing the stress-strain curve is displayed indicating an obvious state of plastic-deformation;2) the failure mode of limestone shows the breakdown of tensile strength from room temperature to 600 °C, as well as the compress shearing damage over 600 °C;3) combining our test results with the concept of thermal damage, a thermal damage equation was derived.

Purification and Characterization of a New Thermostable κ-CarrageenasefromtheMarineBacterium Pseudoalteromonas sp. QY203

A new extracellular κ-carrageenase, namely CgkP, 34.0 kDa in molecular weight, was purified from Pseudoalteromonas sp. QY203. CgkP showed relatively high activity at acidities ranging from pH6.0 to pH9.0 and temperatures ranging from 30℃ to 50℃ with the highest activity at 45℃ and pH7.2. Sodium chloride increased its activity markedly, and KC1 increased its activity slightly. The divalent and trivalent metal ions including Cu^2＋, Ni^2＋, Zn^2＋, Mn^2＋, Al^3＋ and Fe^3＋ significantly inhibited its activity, while Mg^2＋ did not. CgkP remained 70% of original activity after being incubated at 40℃ for 48h, and remained 80% of the activity after being incubated at 45℃ for 1 h. It exhibited endo-κ-carrageenase activity, mainly depolymerizing the κ-carrageenan into disaccharide and tetrasaccharide. CgkP was more thermostable than most of previously reported κ-carrageenases with a potential of being used in industry.

Distribution of Borehole Temperature at Four High-altitude Alpine Glaciers in Central Asia

The distribution of borehole temperature at four high-altitude alpine glaciers was investigated. The result shows that the temperature ranges from -13.4℃ to -1.84℃, indicating the glaciers are cold throughout the boreholes. The negative gradient （i.e., the temperature decreasing with the increasing of depth） due to the advection of ice and climate warming, and the negative gradient moving downwards relates to climate warming, are probably responsible for the observed minimum temperature moving to lower depth in boreholes of the Gyabrag glacier and Miaoergou glacier compared to the previously investigated continental ice core borehole temperature in West China. The borehole temperature at 10m depth ranges from -8.0℃ in the Gyabrag glacier in the central Himalayas to -12.9℃ in the Tsabagarav glacier in the Altai range. The borehole temperature at 10 m depth is 3-4 degrees higher than the calculated mean annual air temperature on the surface of the glaciers and the higher 10 m depth temperature is mainly caused by the production of latent heat due to melt-water percolation and refreezing. The basal temperature is far below the melting point, indicating that the glaciers are frozen to bedrock. The very low temperature gradients near the bedrock suggest that the influence of geothermal flux and ice flow on basal temperature is very weak. The low temperature and small velocity of ice flow of glaciers are beneficial for preservation of the chemical and isotopic information in ice cores.

Climate Change Facts in Central China during 1961-2010

Based on the observations from 239 meteorological stations located in Central China （Henan, Hubei and Hunan provinces）, this paper focuses on the climate change facts during 1961- 2010. There was a significant increasing trend in annual mean temperature for Central China during 1961 -2010. The increasing rate was 0.15℃ per decade, which was lower than the national trend. Since the mid-1980s, temperature increasing was obvious. Large increasing rate was observed in the mid-eastern part of Central China. For the four seasons, the increasing rate in winter was the largest （0.27℃ per decade）. The increasing rate in the annual mean minimum temperature was larger than that in the annual mean maximum temperature from 1961 to 2010. As a result, the diurnal range of temperature decreased at the rate of -0.10℃ per decade. The extreme high temperature events were increasing while the extreme low temperature events were significantly decreasing. There was no obvious trend in annual precipitation for Central China during 1961-2010. Precipitation in summer and winter significantly increased; change of precipitation in spring was not obvious; precipitation in autumn was decreasing. The decreasing rate of annual rainy days was -3.4 d per decade. The precipitation intensity increased at the rate of 0.25 mm d-1 per decade. Heavy-rain days significantly increased. Spring and summer started earlier while autumn and winter started later. As a result, spring and summer duration was expanding whereas autumn and winter duration shortened.

Hot-compression behavior of Al alloy 5182

Hot-compression of aluminum alloy 5182 was carried out on a Gleeble- 1500 thermo-simulator at deformation temperature ranging from 350 ℃ to 500 ℃ and at strain rate from 0.01 s^-1 to 10 s^-1 with strain range from 0.7 to 1.9. The microstructures and macro-textures evolution under different conditions were investigated by polarized optical microscopy and X-ray diffraction analysis, respectively. The basic trend is that the hot-compression stress increases with the decrease of temperature and increase of strain rate, which is revealed and elucidated in terms of Zener-Hollomon parameter in the hyperbolic sine equation with the hot-deformation activation energy of 143.5 kJ/mol. An empirical constitutive equation is proposed to predict the hot-deformation behavior under different conditions. As deformation temperature increases up to 400 ℃, at strain rate over 1 s^-1, dynamic recrystallization （DRX） occurs. Cube orientation { 100} （001） is detected in the recrystallized sample after hot-compression.

The Maximum Temperatures （Tmax） Distribution on the Body Surface of Sport Horses

The objective of the study was to determine the usefulness of measuring maximum temperatures in designated regions of a healthy horse＇s body surface. Thermographic investigations （Thermovision〉550, FLIR） were carried out on 35 horses from 6 to 16 years old participating in show jumping competitions. The rectal temperatures of the horses were in the range 37.5-38.2 ℃. The research was performed in a stable, the ambient temperature （Tab） of which was 14℃ with a humidity （φ） of 60%. Thermograms of the left and right side of the horses were obtained. Each thermogram consisted of 36 body surface regions （before the competition） and 25 regions （immediately after the competition）. The maximum temperature ranges at rest were 21.8 ℃-31.0℃ and symmetrical regions did not differ statistically （P 〉 0.05）. The highest temperatures were on the head, neck and trunk, the lowest-on the limbs. The hind legs were warmer than the front legs in analogous areas, with the exception of the gaskin and forearm. The warmest body areas had the largest surface area, which is indicative of their crucial role in the thermoregulation of the equine organism. The research results may therefore be useful in veterinary diagnosis. The range of maximum temperatures after the competitions was 25.2℃-34.2℃. The highest increment was observed at the breast, elbow, forearm and gaskin, the lowest-at the head, pastern and hoof （foreand hind limbs）. Research regarding body surface temperature after exercise does not have diagnostic value for veterinarians because ＂warming-up＂ certain parts of body surface masks inflammation.

Dielectric anomalies in CaCu_3Ti_4O_(12) at high temperatures

We reported the dielectric properties of CaCu3Ti4O12 in the temperature range from room temperature to 800℃ and the frequency range from 20 Hz to 10 MHz.Apart from the widely reported dielectric anomaly occurring around 200℃,three additional dielectric anomalies were found.The new anomalies are very sensitive to electrode sintering conditions and annealing atmospheres,indicating that they are dependent not only on the electrode-sample contact but also on oxygen vacancies.

Critical minimum temperature limits xylogenesis and maintains treelines on the southeastern Tibetan Plateau

Physiological and ecological mechanisms that define treelines are still debated. It has been suggested that the absence of trees above the treeline is caused by low temperatures that limit growth. Thus, we hypothesized that there is a critical minimum temperature （CTmin） preventing xylogenesis at treeline. We tested this hypothesis by examining weekly xylogenesis across three and four growing seasons in two natural Smith fir （Abies georgei var. srnithii） treeline sites on the southeastern Tibetan Plateau. Despite differences in the timing of cell differentiation among years, minimum air temperature was the dominant climatic variable associated with xylem growth; the critical minimum temperature （CTmin） for the onset and end of xylogenesis occurred at 0.7 ±0.4 ℃. A process-based modelling chronology of tree-ring formation using this CTmin was consistent with actual tree-ring data. This extremely low CTmin permits Smith fir growing at treeline to complete annual xylem production and maturation and provides both support and a mechanism for treeline formation.