《雪暴》的密闭空间美学解读

当代电影注重影片自身的空间营造,通过独特的空间镜语使影片的叙事形成自有的语义,从而传达出影片更加深刻的精神内核,空间美学已然成为电影语言的重要注脚运用在各类影片中,电影中密闭空间的运用是其空间美学的一个重要组成部分,用以增强影片的特殊语境,其在犯罪类型片、恐怖类型片、伦理剧情片中多有涉及。2018年,国产影片《雪暴》获釜山电影节新浪潮大奖,片中密闭空间美学的构建具有独特的视觉观感。

《雪暴》:大雪苍茫 无从留念

【剧情简介】在一座极北的边陲小镇,一伙穷凶极恶、作案手法老到的悍匪为抢夺黄金,打劫运金车,并借助大雪掩盖了所有犯罪痕迹。为了探求真相,警察王康浩暗地里搜集证据、熟悉地形,终于在一场灾难级的暴雪降临时,与谋财害命的悍匪发生了惊心动魄的正面对决……

A case study of cold-seasonthundersnow in Beijing

The characteristics of local thundersnow at ne spatiotemporal scale on 9 and 10 November 2009 in Beijing were analyzed,using wind pro ler,microwave radiometer,automatic weather station,Doppler weather radar,and satellite data.Furthermore,the causes of winter convection are discussed.The results showed that it was reflux weather.The cause of the thunder and lightning was the elevated convection above the lower cold and dry air,and the trigger for convection was the short wave trough and convergencein the middle level.This thundersnow event developed from monsoon-like long-lasting water vapor transport at 850 hPa from the South China Sea along with strong instability of,and convergence in,the conveyor layer.

A Study on Snowstorm Weather in Coastal Area of Western Antarctic

In this paper, based on the observational data of 1995 in the Chinese Antarctic Great Wall Station the snowstorm is studied synoptically. It is found that there are two kinds of snowstorms with different physical characteristics and that the happening of snowstorm is always accompanied by a near-ground level inversion layer. The function of the inversion layer is analyzed, too. It is indicated that the strong ESE-wind type snowstorm is mainly caused by katabatic wind and gradient wind together. This idea is new and different from the general concept that there is no katabatic wind in the western Antarctic area.

Analysis of the extremely cold and heavy snowfall in North America in January 2015

With global warming and declining Arctic sea ice area in autumn observed by satellites since 1979, anomalous cold snaps in recent winters have affected large parts of North America, Europe, and East Asia. In January 2015, North America suffered extremely cold and heavy snowfall events. As revealed in this paper, the NCEP reanalysis data show that the temperature decreased significantly in January 2015 in North America, including the air temperature in the troposphere and the surface air temperature. Moreover, snow cover increased obviously in January 2015 in North America, while there was a significant negative anomaly of geopotential height. The wind formed the anomalous pattern, which favored cold currents blowing to the North American continent from the polar region, and bringing plenty of water vapor. Our results suggest that the anomalous north wind and decreasing westerly jet stream, which allowed cold and moist air to easily penetrate the North American continent from the Arctic, was one of the main reasons for the extremely cold and heavysnow winter of 2015 in North America.

Role of Black Carbon-Induced Changes in Snow Albedo in Predictions of Temperature and Precipitation during a Snowstorm

In this study the authors apply the chemistry version of the Weather Research and Forecasting model （WRF-Chem） to examine the impacts of black carbon （BC）-induced changes in snow albedo on simulated temperature and precipitation during the severe snowstorm that occurred in southern China during 0800 26 January to 0800 29 January 2008 （Note that all times are local time except when otherwise stated）. Black carbon aerosol was simulated online within the WRF-Chem. The model resuits showed that surface-albedo, averaged over 27-28 January, can be reduced by up to 10% by the deposition of BC. As a result, relative to a simulation that does not consider deposition of BC on snow/ice, the authors predicted surface air temperatures during 27-28 January can differ by -1.95 to 2.70 K, and the authors predicted accumulated precipitation over 27-28 January can differ by -2.91 to 3.10 mm over Areas A and B with large BC deposition. Different signs of changes are determined by the feedback of clouds and by the availability of water vapor in the atmosphere.

Johanson-Blizzard syndrome

Johanson-Blizzard syndrome(JBS) is a rare autosomal recessive disease characterized by exocrine pancreatic insufficiency,hypoplastic or aplastic nasal alae,cutis aplasia on the scalp,and other features including developmental delay,failure to thrive,hearing loss,mental retardation,hypothyroidism,dental abnormalities,and anomalies in cardiac and genitourinary systems.More than 60 cases of this syndrome have been reported to date.We describe the case of a male infant with typical symptoms of JBS.In addition,a new clinical feature which has not previously been documented,that is anemia requiring frequent blood transfusions and mild to moderate thrombocytopenia was observed.A molecular study was performed which revealed a novel homozygous UBR1 mutation.Possible explanations for this new association are discussed.

Simulation of a Freezing Rain and Snow Storm Event over Southern China in January 2008 Using RIEMS 2.0

The Regional Integrated Environmental Model System （RIEMS 2.0） with NCEP Reanalysis II is utilized to simulate the severe freezing rain and snow storm event over southern China in January 2008, which caused severe damage in the region. The relationships between the freezing rain process and the large-scale cir- culation, in terms of the westerly and low-level jets, water vapor transportation, and northerly wind area/intensity indices, were analyzed to tmderstand the mechanisms of the freezing rain occurrence. The results indicate the fol- lowing： （1） RIEMS 2.0 reproduced the pattern of precipi- tation in January 2008 well, especially for the temporal evolution of daily precipitation averaged over the Yangtze River valley and southern China; （2） RIEMS 2.0 repro- duced the persistent trough in the South Branch of the westerlies, of which the southwesterly currents trans- ported abundant moisture into southern China; （3） RIEMS 2.0 reasonably reproduced the pattern of frequencies of light and moderate rain, although it overestimated the frequency of rain in southern China. This study shows that RIEMS 2.0 can be feasibly applied to study extreme weather and climate events in East Asia.