冰川

Glaciers on the 12th, also known as "transparent dream Ko" ice, in 1959 by the Chinese Academy of Sciences Research Station of Alpine glacier experts found.

12号冰川，又名&透明梦柯&冰川，于1959年被中国科学院高山冰川研究站的专家们发现。

The SO2-4 and Ca2+, particularly SO2-4, are major ions in snow and ice of snow pits on Haxilegen Glacier No.51 of Kuitun river, where its ion chemistry in snow pits is different from that on Hami Miaoergou FlatTopped Glacier, which is most likely related to the geographical location of Hami Miaoergou FlatTopped Glacier that is located in the leeward site of the Taklimakan desert, Shanshan desert and Gurbantunggut desert, and also probably associated with the elution process in snow pits and altitude effect of deposition flux.

SO42-和Ca2+是奎屯河哈希勒根51号冰川雪坑中的主要离子（尤其是SO42-），其雪坑离子化学特征与哈密庙尔沟平顶冰川差别较大，可能与哈密庙尔沟平顶冰川处于塔克拉玛干沙漠、古尔班通古特沙漠和鄯善沙漠的下风向相关，还可能与雪层内淋融作用的强弱和沉积通量的高程效应有关。

The ion concentrations were studied in both four snow pits on Hami Miaoergou FlatTopped Glacier and one snow pit on Haxilegen Glacier No.51 of Kuitun river in eastern Tianshan Mountain, and both snow pits were retrieved in 2004. The results show that the Ca2+, NO-3 and SO2-4, particularly Ca2+, are major ions in the snow of snow pits in both ablation and accumulation area and also in the ice of snow pits in accumulation area on Hami Miaoergou FlatTopped Glacier, where the relationships among major cation concentrations in snow of snow pits can be revealed by ion concentrations in the ice of snow pits, but the correlation between ion concentrations in the snow of snow pits and elevation is not obvious, which probably can be attributed to the narrow span of elevation and sparse snow pits on glacier. However, the good correlation between ion concentrations in the ice of snow pits and elevation indicates that the elution process weakened gradually with the elevation rise and temperature decrease.

对2004年获取的天山奎屯河哈希勒根51号冰川1个雪坑和哈密庙尔沟平顶冰川4个雪坑的离子浓度特征进行了研究，结果表明：Ca2+、NO-3和SO42-是哈密庙尔沟平顶冰川雪坑雪层和积累区雪坑底部冰中的主要离子（尤其是Ca2+），其雪层中的主要阳离子关系可在底部冰中得以较好的反映，但雪层中各离子浓度与海拔的相关性不明显，可能与海拔的跨度较小和挖取的雪坑较疏有关；雪坑底部冰中的离子浓度与海拔间明显的相关性说明淋融作用随着海拔升高、气温降低而逐渐减弱。

The glacier grows against wind. The larger the glacier grows on slope facing wind, the less the moisture air is advected to another side. The glaciers are hard to grow on another side. Thus, the snow line on the slopes facing wind is lower than on the opposite side.For the ice sheets at LGM, the climate drivers are the surface air temperature, relative sea level change and ELA at LGM. Two ELA were reconstructed. One is the altitudes of ancient cirques, and another is the height difference at 0oC level between July and May.

构建了2种ELA，一种为古冰斗、冰碛陇的高度，另一种为由7月、5月0oC层的高度差得到的ELA，分别与复原的该时期的年平均空气温度和该时期的海平面高度，构成2种外部强迫方案，对LGM时期青藏高原冰川的覆盖程度进行了模拟，对有无统一大冰盖重新进行了评估。2种模拟结果发现，尽管高原的东南部和西北部冰川分布较集中，但仍有独立的冰川中心存在，并未形成统一大冰盖。

The conversions of ice temperature and ice velocity occur from bridge to trough of terrain on the eastern Nyainqentanglha Range. The ice temperature at bridge is lower. The ice at bridge starts to move due to the larger gravitational driving stress. During the course from bridge to trough of terrain, basal ice temperature rises because of the friction. While reaching the pressure melting point of ice, basal decollement occurs, and higher velocities can still be produced at trough.

而位于念青唐古拉山东部地区的冰川，冰温和冰速从地形脊到地形槽处发生了较大的转化过程，在地形脊处冰温较低，受重力加速度的影响，冰川开始产生滑动，从地形脊到地形槽滑动的过程中，其底部受摩擦加热的影响，底部冰温升高，达到融化点，底部产生变形，到地形槽处仍会产生较大速度的滑动，因此冰川的运动从地形脊到地形槽处发生了转化，即地形脊处的滑动属动力过程引起的滑动，而地形槽处的滑动属热力过程产生的滑动。

The Ice Age was a long period of time in which four great glaciers pushed southward...

五大湖区与三河水域的形成以及四大冰川都只是冰川都只是冰川时代的一部分，故、与错。

The ongoing Extreme Ice Survey hopes to shed some light on why these so-called tidewater glaciers, which end in water instead of land, are being lost at such a rapid rate.

正在进行的&极度冰川调查&项目，就是要给人们提供证据：为什么被称为潮水冰川（消失在潮水中而非陆地上）的冰川正在以如此快的速度消逝着。

Forest of seracs is a kind of ice-surface landform in ablation areas of continental glaciers.

冰塔林是大陆性冰川消融区的一种冰面地貌，我国主要在珠穆朗玛峰北坡的冰川和喀喇昆仑山的冰川上有发育，这是中低纬度地区太阳直射对冰面产生的差别消融侵蚀，从而形成的一种奇特的冰面地貌。

Forest of seracs is a kind of ice-surface landform in ablation areas of continental glaciers, in China mainly developed in glaciers on north face of Mount Qomolangma and on the Karakorum Mountains. This kind of surprising tower-or-forest-liked ice-surface landform is caused by different ablation erosion happened on ice surfaces with vertical sunrays in middle and lower latitude areas.

冰塔林是大陆性冰川消融区的一种冰面地貌，我国主要在珠穆朗玛峰北坡的冰川和喀喇昆仑山的冰川上有发育，这是中低纬度地区太阳直射对冰面产生的差别消融侵蚀，从而形成的一种似塔似林的奇特冰面地貌。

Forest of seracs is a kind of ice-surface landform in ablation areas of continental glaciers, in China mainly developed in glaciers on north face of Mount Qomolangmaand on the Karakorum Mountains. This kind of surprising tower-or-forest-liked ice-surface landform is caused by different ablation erosion happened on ice surfaces with vertical sunrays in middle and lower latitude areas.

冰塔林是大陆性冰川消融区的一种冰面地貌，我国主要在珠穆朗玛峰北坡的冰川和喀喇昆仑山的冰川上有发育，这是中低纬度地区太阳直射对冰面产生的差别消融侵蚀，从而形成的一种似塔似林的奇特冰面地貌。

Since historical times,England ,where the early inhabitants were Celts, has been conquered three times .

从有历史以来，英国，在此地早期居住的是凯尔特人，已经被征服了三次。

Bluetooth OBEX File Transfer Enables the sending and receiving of files on your phone via Bluetooth.

蓝牙OBEX文件移动允许经过蓝牙传送和接受文件。。。。