一部赞美黑龙江冰雪文化 弘扬少数民族文明的佳作——读《冰雪文化与黑龙江少数民族》

2008年,龚强先生的新作《冰雪文化与黑：龙江少数民族》一书由黑龙江人民出版社出版了。这是一部系统展示冰雪文化和黑龙江世居少数民族风情及其内在联系的著作。这部书全面记述了冰雪文化的形成与演进,阐释了冰雪文化在中华文明中的地位和作用;对10个世居于黑龙江流域的少数民族做了全方位的展示和介绍,颂扬了他们创造并丰富冰雪文化的开拓创新精神,讴歌了他们对冰雪文化所做出的卓越贡献。透过浓郁的少数民族风情可以领略到冰雪文化的源远流长,综观黑龙江少数民族的历史足迹能够了解到冰雪文化的厚重与深邃。     

满族冰雪文化特征探析

冰雪文化是人类认识和改造冰雪所获得的全部成就的总和,包括物质和精神两个方面。地处白山黑水的满族人与冰雪结下不解之缘,所创造的冰雪文化从内容上看:冰雪娱乐和运动的习俗是满族冰雪文化的核心。满族冰雪文化具有地域性、观赏性、包容性、军体性等特征。     

冰情雪韵话图志——评《黑龙江冰雪文化图志》

<正>天一天地冷,冰雪一天一天地热,冰雪旅游也随之一天一天地升温。冰雪孕育着文化,文化揭示了冰雪无穷的魅力。随着读图时代的到来,黑龙江省地方志编纂委员会在继承传统的基础上精心编制了《黑龙江冰雪文化图志》(以下简称《图志》),以独特的文化视角,全方位多角度深层次地展示了黑龙江冰雪文化的产生、普及与发展的历史和现状, 将冰情雪韵以图文并茂的形式展示给读者,同时也是献给广大读者的一道富有浓厚文化底蕴和地域特色的冰雪文化大餐。     

一部赞美黑龙江冰雪文化 弘扬少数民族文明的佳作——读《冰雪文化与黑龙江少数民族》

<正>2008年,龚强先生的新作《冰雪文化与黑龙江少数民族》一书由黑龙江人民出版社出版了。这是一部系统展示冰雪文化和黑龙江世居少数民族风情及其内在联系的著作。这部书全面记述了冰雪文化的形成与演进,阐释了冰雪文化在中华文明中的地位和作用;对10个世居于黑龙江流域的少     

土乡风俗冰雪情

＂冰雪高原醉美互助欢乐土乡＂——每年给您一个不一样的冰雪世界。彩虹部落文化旅游发展有限公司在成功举办两届冰雪文化节的基础上,将举行青海互助第三届冰雪文化欢乐节。本次冰雪节将推出十大冰雪项目、四个具有民族特色的观赏及参与项目,使您充分体验冰雪文化所带来的快乐。     

黑龙江冰雪文化礼赞(二)——冰雪资源抒怀

千百年来,全世界的劳动者创造了许许多多灿烂的文化,这些文化如群星闪烁,璀璨耀眼.而就冰雪文化而言,黑龙江省是重要的发祥地,是我国冰雪文化的发源地.黑龙江冰雪资源堪称全国之最,每逢冬季,天公作美,玉女散花,瑞雪普降,片片雪花,纷纷扬扬,飘落人间.     

黑龙江冰雪文化礼赞(五)——鄂伦春人·游猎·民间艺术

自然环境、民俗风情是地域文化形成和发展的重要因素.黑龙江灿烂的冰雪文化,首先源于大自然恩赐给我们的严冬与冰雪,而由自然冰雪升华成冰雪文化,则是世世代代居住在这块神奇土地上的各族人民拼搏、创造、传承、发展的功绩.历史上黑龙江流域多民族文明的不断发展,使得黑龙江具有博大、深厚、丰富的多民族文化底蕴.在黑龙江世居的10个常年与冰雪为伴的少数民族中,鄂伦春族是最具特色的少数民族之一.他们在漫长的发展进程中,在生产、生活和社会实践中,创造了丰富的物质文化和灿烂的精神文化.风霜雨雪铸就了他们坚毅、热情、果敢、豪放的性格,广阔天地培养了他们大气、粗犷、泼辣、率真的品质.尤其是他们创造的游猎文化、桦皮雕刻、皮板刺绣、舞蹈艺术是黑龙江冰雪文化中的瑰宝.正是由于鄂伦春人这些彪炳显赫的历史贡献,使黑龙江冰雪文化更加多姿多彩,更加富有神韵,更加魅力无穷,更加灿烂辉煌.     

浅谈冰雪雕塑的造型艺术

冰雪雕塑又可称之为冰雕艺术,是我国北方地区一种独特的艺术形式,尤其是近些年来,随着冰雪旅游文化的兴起,也进一步推动了冰雪雕塑艺术的蓬勃发展,成为世界性的文化产业。因此,本文笔者从冰雪雕塑的艺术造型特点,艺术审美价值入手,对冰雪雕塑进行粗浅的分析,以期解析更多的冰雪雕塑造型艺术特点。     

《阿勒泰冰雪文化志》篇目研讨会召开

2021年6月15日,《阿勒泰冰雪文化志》篇目研讨会在自治区地方志编委会召开。编委会党组书记、副主任廖运建,一级巡视员刘星,阿勒泰地区地方志办公室主任田宏波,《阿勒泰冰雪文化志》编写办公室相关工作人员,编委会地县工作处相关负责人等参加。廖运建主持会议。编写办公室主任黄天翔介绍《阿勒泰冰雪文化志》篇目形成及初稿编纂过程。与会专家根据志书编纂的要求,立足阿勒泰冰雪文化的实际,对篇目提出修改意见和建议,就《阿勒泰冰雪文化志》篇目框架和编纂中遇到的具体问题进行探讨、交流。     

乌鲁木齐打造丝绸之路冰雪旅游品牌

2007年12月26日,乌鲁木齐市举办第五届“丝绸之路冰雪风情节”。据市旅游局旅游党组书记梁治龙介绍,该市30多家滑雪场全力迎接游客,日接待游客能力达到了2,5万人次。此外,包括举办冰雪艺术活动、冰雪体育活动、冰雪文化活动、冰雪旅游在内的活动丰富多彩,冰雕游园、冬泳表演、群众性冬季长跑、冰雪集体婚礼以及各种滑雪滑冰旅游活动,为特色浓郁的丝绸之路冰雪旅游增了添魅力。     

黑土文化的剖析与再造

本文从黑土文化概念认识出发,针对以黑龙江省为主体的黑土文化圈进行了文化生态剖析及文化特性阐释。并进而提出了黑土文化时代再造的原则,指出了挖掘文化低韵,重塑外来文化,建构冰雪文化的三大文化再造的主体方向。     

黑龙江省冰雪旅游开发战略AHP决策分析

运用AHP层次分析法,对黑龙江省的冰雪旅游开发战略进行了定性与定量相结合的分析,并得出结论:黑龙江省应该首先实行冰雪旅游产业化战略目标,同时不可忽视冰雪旅游国际化战略目标;而争创品牌战略是第一重要的发展战略;当前亟待解决的首要问题是思想观念不够开放、经济欠发达和管理体制较落后,应该采取的措施是加大体制改革力度、根本改变"多头管理、政令不一"的现状,借鉴国内外冰雪旅游开发成功经验,大力发展滑雪旅游等。通过这些具体措施,可以确保实现"提高黑龙江省冰雪旅游的综合竞争力,把黑龙江省建设成为中国最大、世界知名的冰雪旅游胜地"的总体目标。     

哈尔滨市创建世界冰雪旅游名城对策研究

建设世界冰雪旅游名城已成为新世纪初哈尔滨市实现跨越式发展的一项重要战略举措,如何发展冰雪旅游,做好冰雪旅游产业文章,真正将哈尔滨建设成为国际知名的冰雪旅游城市,是哈尔滨面临的重大课题。本文提出按国际水准进行规划、构建“政府主导社会参与市场运作”发展格局、走“提质增效”的经营道路、推进产品创新、制定有效的市场营销策略、营造世界冰雪旅游名城环境氛围、提升旅游服务、重视人才培养实施人才兴旅战略等相应对策。     

Causes and Factors of Ground-Ice Formation

The concept of ground ice is expanded to cover all forms of ice formed at the interface between two environments—the solid state and the gaseous. Ground ice is thus defined as the product of the layer-by-layer freezing of liquid water or droplets of any origin as it passes from a zone of positive temperatures into a zone below the freezing point. Ground ice may be produced by subsurface waters (springs and groundwater), surface waters (river, lake, sea, glacier and snow meltwater) and atmospheric moisture (glaze, rime, hail). [The definition excludes ice formed within the solid-state environment of the lithosphere (segregated ice, cement ice, injection ice).] Ground ice produced by subsurface waters may be formed at the surface or in large subterranean cavities, and it may be associated with the natural discharge of water or with the freezing of aquifers. Ground ice produced by surface waters may be associated with an increase of water volume in a waterbody as the level of the ice cover remains stable; with a constriction of the discharge cross section, and with changes in heat and moisture exchange. Ground ice derived from atmospheric moisture is formed either on terrestrial objects (glaze, rime) or in the free atmosphere (hail, ice formed on aircraft).     

Effect of multipath and snow on millimeter wave scintillations on a 4.1-km line-of-sight link

Multipath propagation can occur for various reasons. For example, it can be due to sudden changes in the refractive index of the propagation medium or to reflections from melting snow/ice. We find that dry snow, or even ‘moist’ snow at 0°C, has no measurable effect on the propagation of radio waves up to at least 54.5 GHz. When multipath propagation occurs, the low frequency part of the scintillation spectrum is distorted. The usual theoretical predictions applicable to line-of-sight millimeter wave propagaton through clear air turbulence must be used with caution when the scintillations of the propagating signals are a result of multipath effects. It is also noted that propagation through vegetation greatly distorts the clear-air scintillation spectrum. Saturation of scintillations, which can also dramatically alter the scintillation spectrum, is not expected to be a problem for millimeter wave propagation over line-of-sight paths.     

Changes in the Ice Boundary of the Vestfold Hills,East Antarctica, 1947 to 1990

The position of the ice boundary around the Vestfold Hills, East Antarctica (68°30'S, 78°00'E) was observed using a 43 year record of aerial photography from 1947 to 1990. The southern boundary, formed by Sørsdal Glacier, showed two main areas of ice retreat and no areas of advance. Stagnation and retreat of this boundary is interpreted to be contraction to former limits following the Chelnok Glaciation which occurred 7lt; 700 years BP. The eastern or continental ice sheet boundary showed five sites of rapid, localised incision and downwasting around supraglacial gullies. While no area of continental ice was noted to advance, continued accumulation and firnification of wind-drifted snow in the proglacial zone of the ice sheet in the southeastern corner of the hills may signify a locally positive ice mass balance. Until ice mass balance studies are carried out in the ablation zone surrounding the hills, evidence concerning whether the ice sheet boundary is retreating, stable or advancing will remain equivocal.     

The last glaciation in the Western Mourne Mountains,Northern Ireland

During the late‐Midlandian (25–13 ¹⁴C ka BP), the last Irish Ice Sheet was thicker in the Western Mourne Mountains than previously argued. Geomorphological and sedimento‐logical analysis shows that regional ice from the Irish Ice Sheet spilled over the mountains, reaching a major limit 5 km along Pigeon Rock Valley. These findings differ from the previous view that a local valley glacier occupied the valley during this period. The pattern of deglaciation was reconstructed using glacial and periglacial evidence. A complex topographic environment in the upper reaches of the valley suggests that regional ice stagnated as it wasted away. During the Nahanagan Stadial (Younger Dryas, ca. 11–10 ka ¹⁴C BP) an arcuate ridge was formed on the western flank of the valley. Calculations suggest that the Equilibrium Line Altitude, influenced by topographic conditions favourable for snow accumulation, was approximately between 1736 m and 1386 m lower during the Nahanagan Stadial than at present.     

The Silverton Field Experience: a model geography course for achieving high-impact educational practices (HEPs)

High-Impact Educational Practices (HEPs) are a set of specific teaching and learning approaches proven effective in university education. This paper focuses on the benefits derived from utilizing three particular HEPs (inquiry-based collaborative activities, undergraduate research, and experiential learning) while teaching a snow and ice field course titled “Silverton Field Experience.” Student evaluations and instructor feedback reinforce the notion that HEPs encourage deep learning. Deep learning is manifest through increased enthusiasm and participation as well as learning in ways that are meaningful, creative, and stimulating. In terms of pedagogy in geography, these HEPs also create an expanded sense of place and a new way to encourage spatial thinking. The HEPs outlined here are replicable in different geography sub-disciplines and among different settings in higher education and prove exciting to an audience of pedagogic researchers and teacher-practitioners in geographical education.     

JIULONG,LAND OF FAIRY TALES

The area is situated at the end of the land's snow line,along the southern part of Mt. Gonggya(the "Mountain King in Sichuan Province") and at the intersection of Panchi Hua, Xichang Plain, and the Qinghai-Tibet Plateau.     

PROBLEMS IN APPLIED GEOGRAPHY IN CONNECTION WITH THE BAYKAL-AMUR MAINLINE RAIL PROJECT

A discussion of the various environmental impacts of the BAM and of the role of geographers in anticipating and preventing them. Intermontane basins offer relatively favorable areas for settlement, but lack of ventilation rules out the location of polluting industries. Avalanches, ground ice and snow drifting pose particular problems along the route, requiring special-purpose investigations and control measures. A mapping program is proposed to identify farming areas with the most favorable heat supply. A system of geographical field stations is needed to study environmental modification on the ground. Recommendations are made for optimal approaches to settling the BAM zone, distinguishing three categories of population groups: railroad workers, miners and lumbering personnel. Preservation of the indigenous hunting and reindeer economy is urged because of the importance of furs for exports and the use of reindeer as pack animals. Portions of the natural landscape are to be preserved for scientific purposes and, ultimately, for tourism as natural monuments.