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1.
Reconstructed annual net accumulation from the Dasuopu ice core recovered in Himalayas, with a good correlation to Indian monsoon, reflects a major precipitation trend in central Himalayas. The Dasuopu accumulation (DSP An) also shows a strong correlation to the Northern Hemispheric temperature. Generally, as the Northern Hemispheric temperature increases by 0.1 K, the accumulation decreases by about 90 mm and vise versa. Under the condition of global warming, especially since 1920, the Northern Hemispheric mean temperature has increased by about 0.5 K, whereas accumulation in Dasuopu ice core has decreased by about 450 mm. According to the relationship between accumulation and temperature, a scenario prediction of monsoon rainfall in central Himalayas is made. 相似文献
2.
Keqin?Duan "mailto:kqduan@ns.lzb.ac.cn " title= "kqduan@ns.lzb.ac.cn " itemprop= "email " data-track= "click " data-track-action= "Email author " data-track-label= " ">Email author Ninglian?Wang Jianchen?Pu 《科学通报(英文版)》2002,47(8):691-696
Three ice cores distributed across Dasuopu glacier in Himalayas were recovered. A 400-year net annual accumulation record reconstructed from one of the cores reflects the major precipitation trend in the central Himalayas. This record is related closely to the Indian monsoon precipitation. Wavelet and moving T-test were applied to the 400-year-long Dasuopu accumulation record, and significant staggered variability and abrupt change of the record on interannual to centennial time scales are identified. Finally the possible reason for abrupt change of the accumulation record is discussed. 相似文献
3.
Concentrations of Pb in Dasuopu ice core in the Qinghai-Tibetan Plateau have been directly measured by ICP-MS at pg/g level. The Pb profile shows a very significant increase in modern times due to anthropogenic input. The use of leaded gasoline in the South Asian countries may be a main source of Pb in this region. The input of Pb to the Dasuopu Glacier is mainly supplied by Indian summer monsoon moisture which traverses the pass at the head of the Dasuopu Glacier. 相似文献
4.
Fig. . Annually variations of NO-concentration in the Guliya ice core in the period of through AD. 《科学通报(英文版)》2000,45(23):2118-2125
Whether the solar activity was very low, and especially whether the solar cycle existed, during the Maunder Minimum (1645–1715 AD), have been disputed for a long time. In this paper we use the Guliya NO3 − data, which can reflect the solar activity, to analyze the characteristics of the solar activity during the Maunder Minimum. The results show that the solar activity was indeed low, and solar cycle displayed normal as present, i.e. about 11a, in that period. Moreover, it was found that the solar activity contains a 36-year periodic component probably, which might be related to the variations in the length of the sunspot cycle. This finding is of importance for the study of the relationship between the sun variability and the Earth climate change. 相似文献
5.
The variations of NO+--3 concentration in the Guliya ice core are reconstructed for recent about 1 000 a. Spectrum analysis of NO+--3 indicates significant periodicities in the variations of NO+--3 concentration, which coincide with the periodicities of the solar activity. Therefore, a positive correlation between the variations of NO+--3 concentration and the solar activity is found. 相似文献
6.
Ice formation was studied on the Dasuopu Glacier located in the Mount Xixabangma (28°23′ N, 85°43'E) in the Himalayas. Snow pits and shallow ice cores are analyzed to reveal ice formation process. The results show that the ice formation process, or in other words, the process of densitifica-tion, on the col (7 000 m a.s. I.) of the Dasuopu Glacier is a stable, slow and gradual process. The snow-ice transformation on the glacier is estimated to be 30-40 m below the surface. The temperature on the Dasuopu Glacier is very low (～ - 14℃ at 10 m) and similar to that in polar type ice cap. We, therefore, speculate that the process of snow-ice transformation is undertaken under snow pressure, and that there is a percolation zone on the Dasuopu Glacier. The high altitude of the col and monsoon snow fall accompnied by heavy cloud and high albedo favorite the percolation zone formation. 相似文献
7.
Ninglian Wang Tandong Yao L. G. Thompson K. A. Henderson M. E. Davis 《科学通报(英文版)》2002,47(17):1422-1427
Evidence for the “8.2 ka cold event” has been provided mostly from the circum-North Atlantic area. However, whether this cold event occurred in other places is a key to understanding its cause. Here, we provide the evidence for the “8.2 ka cold event” from the Guliya ice core in the northwest Tibetan Plateau, and it was found that the peak cooling (~8.3—8.2 ka) in this ice core was about 7.8—10℃, which was larger than the cooling in the North Atlantic region. The primary causes for this episode were diminished solar activity and weakened thermohaline circulation. Moreover, another weak cold event, centered about 9.4 ka, was also recorded in the Guliya ice core record. These two cold events were concurrent with the ice-rafting episodes in the North Atlantic during the early Holocene, which implies that the millennial-scale climatic cyclicity might exist in the Tibetan Plateau as well as in the North Atlantic. 相似文献
8.
Three ice cores recovered from the Himalayas (i.e. the East Rongbuk Glacier and the Far East Rongbuk Glacier at Mt. Qomolangma (Everest), and the Dasuopu Glacier at Xixiabangma) show a sharp decline in the accumulation rates since the 1950s, which is consistent with the precipitation fluctuation over India and the low northern latitude zone (5°-35°N). Correspondingly, an increasing trend is observed for the ice core accumulations from the central and northern Qingh ai-Tibetan Plateau (i.e. the Xiao Dongkemadi Glacier in the central Tanggula Mountains, the Guliya Ice Cap in the western Kunlun Mountains, and the Dunde Ice Cap in the Qilian Mountains) since the 1950s, which is consistent with the precipi tation fluctuation over the middle-high northern latitude zone (35°-70°N). However, the variation magnitude of the high-elevation ice core accumulations is more significant than that of precipitation at the low-eleva- tion places, suggesti ng its extra sensitivity of high-elevation areas to climatic change. The inter-d ecadal abrupt change of the African-Asian summer monsoon in the1960s may attribute to the recent ice core accumulation change during the recent decades. 相似文献
9.
ZHANG YongJun KANG ShiChang QIN DaHe GRIGHOLM Bjorn MAYEWSKI Paul A. 《科学通报(英文版)》2007,52(23):3261-3266
Annual accumulation records covering 1935 to 2004 were reconstructed using Geladaindong ice core in the source of Yangtze River. A significant positive correlation between annual accumulation and precipitation from nearby meteorological stations was found, suggesting ice core accumulation could be taken as a precipitation proxy in the region. In the past 70 years, precipitation in the Geladaindong region was low from 1930s to early 1960s, and the lowest value occurred in the later 1950s. Since 1960s, precipitation increased dramatically and reached the maximum around 1980s, then decreased slightly in 1990s. By using Mann-Kendall rank statistical test method, a change point for precipitation was determined in 1967. Analysis of the atmospheric circulation over the Tibetan Plateau suggested that, compared with the southwest wind during the low precipitation period （before 1967）, it extended about 2 latitudes northward during high precipitation period （after 1967）. Moreover, during the high precipitation, the trough over the Bal Karshi Lake was also enhanced, and both the meridional wind and vapor transporting displayed a remarkable aggrandizement. 相似文献
10.
ZHANG Mingjun LI Zhongqin XIAO Cunde YANG Huian KANG Jiancheng LI Jun 《自然科学进展(英文版)》2001,11(7):525-528
A 50 m firn core drilled in Princess Elizabeth Land, Antarctica, during the 1996/1997 Chinese First Antarctic Inland Expedition, has been measured for б18O and major ions. Based on these data, the features of the climate change in the investigated region in the past 250 years have first been studied. In the past 250 years, the change trend of climate in this region can be divided into two periods by the year 1860. Both the temperature and accumulation rate display increasing trend before 1860, while after 1860, the decreasing trend of the temperature is obvious but the change of the accumulation rate is not clear. Although both the temperature and the accumulation rate are increasing in the past 50 years, they are not the highest values in the past 250 years. So it is clear that the climate change in this region during this period does not reflect recent global wanning. 相似文献
11.
TIAN LiDe YAO TanDong WU GuangJian LI Zhen XU BaiQing LI YueFang 《科学通报(英文版)》2007,52(10):1436-1439
The total activity variation with depth from a 41.6 m Muztagata ice core drilled at 7010 m, recorded not only the 1963 radioactive layer due to the thermonuclear test, but also clearly the radioactive peak released by the Chernobyl accident in 1986. This finding indicates that the Chernobyl nuclear accident was clearly recorded in alpine glaciers in the Pamirs of west China, and the layer can be potentially used for ice core dating in other high alpine glaciers in the surrounding regions. 相似文献
12.
杜九林 《陕西师范大学学报(自然科学版)》1999,27(3)
研究了８ Ｂ中微子产生过程中存在时间振荡的动力学判据． Ｈｏｍ ｅｓｔａｋｅ 实验记录的太阳中微子流具有时间周期性,而 Ｓｕｐｅｒ Ｋａｍ ｉｏｋａｎｄｅ 实验观测的太阳中微子流基本上是恒定的．这一矛盾的合理解释可能是太阳中心中微子的产生率具有长的时间振荡周期 相似文献
13.
异常的第24太阳活动周——新千年的第一个完整的太阳活动周 总被引：2，自引：0，他引：2
介绍自2007年下半年到现在的非常低的太阳活动状况:无黑子活动天数为16太阳活动周以来最多,不排除24周的无黑子天数是现代黑子周内最多的可能;高纬度(35°)黑子的纬度为12周最低;从2003年11月～2008年9月,较高纬度(20°)每月没有黑子或只有1个黑子,共计持续了58个月,也为12周以来第一次观测到;太阳风速度、太阳风压、10cm电磁波辐射、太阳极区磁场、太阳总光度辐射等参量都为有观测资料以来的最低.对于这种极低太阳活动的现象,介绍了从当前的日震观测给予的解释、也从Gleissberg周期的长尺度、超长太阳活动周期尺度给予了解释.依据目前的观测,我们确定24黑子活动周于2008年11月开始.综合多种经典太阳活动预报方法给出的对24周太阳活动水平的预报,以及美国国家航空航天局和美国国家海洋大气局对24周的未来发展趋势的预报,认为24周太阳活动水平估计比23周将要弱30%左右.异常的24太阳活动周为太阳物理和日地关系物理研究带来机遇. 相似文献
14.
于不同季节采集样品１８１种．分离获得３７５株细菌并采用经Ｌｉｎｄｏｗ修改的方法进行冰核活性测定，结果有２０株活性较高．并对其活性最高的２５６号菌株进行分类鉴定，归类为欧文氏菌的草生群 相似文献
15.
改进型太阳能固体吸附式制冰机的研制 总被引：7，自引：1，他引：7
基于平板式太阳能制冰机的大量实验研究及理论分析计算,对太阳能固体吸附式制冰机进行了新一轮的优化设计,各子部件采用无阀连接结构,使系统操作更为简单,实验表明,系统的吸附床、冷凝器、蒸发器等子部件之间性能匹配良好,设计制作的实物样机从工艺及制造成本上均接近产业化生产的要求,为太阳能固体吸附式制冷的民用化应用提供了依据。 相似文献
16.
XiangBin Cui Bo Sun Gang Tian XueYuan Tang XiangPei Zhang YunYun Jiang JingXue Guo Xin Li 《科学通报(英文版)》2010,55(4-5):425-431
Dome A, located in the central East Antarctic ice sheet (EAIS), is the highest summit of the Antarctic ice sheet. From ice-sheet evolution modeling results, Dome A is likely to preserve over one million years of the Earth’s paleo-climatic and -environmental records, and considered an ideal deep ice core drilling site. Ice thickness and subglacial topography are critical factors for ice-sheet models to determine the timescale and location of a deep ice core. During the 21st and 24th Chinese National Antarctic Research Expedition (CHINARE 21, 2004/05; CHINARE 24, 2007/08), ground-based ice radar systems were used to a three-dimensional investigation in the central 30 km×30 km region at Dome A. The successfully obtained high resolution and accuracy data of ice thickness and subglacial topography were then interpolated into the ice thickness distribution and subglacial topography digital elevation model (DEM) with a regular grid resolution of 140.5 m×140.5 m. The results of the ice radar investigation indicate that the average ice thickness in the Dome A central 30 km×30 km region is 2233 m, with a minimal ice thickness of 1618 m and a maximal ice thickness of 3139 m at Kunlun Station. The subglacial topography is relatively sharp, with an elevation range of 949–2445 m. The typical, clear mountain glaciation morphology is likely to reflect the early evolution of the Antarctic ice sheet. Based on the ice thickness distribution and subglacial topography characteristics, the location of Kunlun Station was suggested to carry out the first high-resolution, long time-scale deep ice core drilling. However, the internal structure and basal environments at Kunlun Station still need further research to determine. 相似文献
17.
18.
Carbonaceous particles concentrations of OC and EC are determined using a two-step gas chroma- tography system in Muztagh Ata ice core covering the time period of 1955--2000. Over the period represented by the core, OC and EC concentrations appear to have changed significantly, varied in the range of 17.7--216.7 and 6.5--124.6, and averaged 61.8, 32.9 ng·g^-1, respectively. The average concentration of EC in Muztagh Ata ice core is much lower than that in an Alpine ice core record （100--300 ng·g^-1） during the same period, but it is a factor of 14 in Greenland ice core （2.3 ng·g^-1）, this may induce a strong impact on the snow albedo in the last 46 years in our study area. Observations indicate two periods with obviously high deposition concentrations （1955--1965 and 1974--1989） and two periods with low concentrations （1966--1973 and 1990--1995）, as well as a recent increasing trend. By comparing EC and SO4^2- concentration variations and deciphering OC/EC ratios recorded in the same ice core, we can judge roughly that the carbonaceous particles deposited in Muztagh Ata ice core were attributed to fossil fuel combustion sources. 相似文献
19.
Based on the oxygen isotope ratio and microparticle record in ice cores recovered at Mt. Muztagata, Eastern Pamirs, the seasonal variations of atmospheric dust have been reconstructed for the past four decades. High dust concentrations and coarser particle grains have the similar trend with oxygen isotope value. Our statistical results indicate that 50%--60% high dust concentration samples occur during the season with high oxygen isotope values （summer）, while low dust storm frequency during spring and winter. Back-trajectory analysis shows that the air mass hitting Muztagata predominately came from West Asia （such as Iran-Afghanistan Plateau） and Central Asia, which are the main dust source area for Muztagata. Dust storms in those source areas most frequently occur during summer （from May to August）, while frequent dust storm events in northern China mainly occur during spring （March to May）. Regions in the path of Asian dust transport, such as in Japan, the North Pacific, and Greenland, also show high dust concentrations during spring （from March to May）. Our results indicate that dust storms have different seasonality in different regions within Asia. 相似文献
20.
Based on the Guliya ice core records, the precipitation in the past 400 years was retrieved. Its rela tions with other regions were also analyzed. The results demonstrated that there were two high-precipitation periods and two low-precipitation periods in Guliya ice core since 1571 AD. The average precipitation in the two high-precipitation periods was 42 mm (21%) higher than that in the two low-precipitation periods. The precipitation recorded in the Guliya ice core was consistent with that in Dunde ice core. The variation trends of precipitation in the Guliya ice core and the northern hemisphere are similar. During the extremely wet years in the northern hemisphere, the precipitation recorded in the Guliya ice core was two times the long-term average. However, the annual precipitation was 38% less than that of the long-term average in extremely dry years. 相似文献