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- The Improvement of Artificial Ice Crystal Parameterization of IAP Three-Dimensional Convective Storm Model and Its Application to Case Study 三维对流云催化数值模式人工冰晶参数化方案的改进与个例模拟试验
- artificial ice crystals 人工引晶
- Ice crystals begin to deform measurably. 冰晶就产生某种程度的变形了。
- Artificial ice crystal 人工冰晶
- Cirrus is formed from ice crystals. 卷云是冰晶形成的。
- Snowflakes are loose aggregates of ice crystals. 雪花是冰晶的松散凝结。
- Ice: Three ice crystals will protect the sorceress. 冰晶：制作出三个冰晶来保护女巫。
- Light pillars appear when artificial light (shown in diagram above) or natural light bounces off the facets of flat ice crystals wafting relatively close to the ground. 光柱出现是人工光源（图所示以上）或自然光由冰晶的小平面反射而飘到相对近的地面上。
- Atmospheric Ice Crystals over the Antarctic Plateau in Winter. 冬季南极高原大气冰晶。
- Though light pillars are often caused by artificial light, sun pillars, as in the above picture, occur when sunlight reflects off the facets of millions of flat ice crystals in very cold air. 虽然光柱往往是人工光源造成，如上述图片，当阳光在极冷的空气中从侧面通过数以百万计的单位冰晶反射便形成了太阳光柱。
- No bells rang, no ice crystals appeared on the bulkheads, nothing changed. 既没有警铃响起，也没有冰晶在隔水舱壁上凝结，一切如常。
- Ice crystal number concentration versus temperature for climate studies. 冰晶数的集中对应气候研究的温度。
- Scientists believe that tiny ice crystals of nitric acid in Antarctica's upper atmosphere are directly involved. 科学家认为，南极上部大气圈内微小的硝酸冰晶也直接参与其中。
- A deposit of minute ice crystals formed when water vapor condenses at a temperature below freezing. 霜冻当气温低于零度时由水蒸气凝结而成细小冰晶的沉积
- Its origin is required of refraction or reflection of the light by atmospheric ice crystals. 它是由大气的冰晶对光的折射或反射所产生的。
- As the basic form of ice crystals is a hexagonal prism, most ice crystals are six-sided in shape at the beginning. 由于冰晶的基本模式是六角棱体,大部份冰晶的雏形都是六角形的。
- If we want to understand why most ice crystals are hexagonal prisms, we should study water molecules first. 若果我们希望找出大部分冰晶是六角棱体的原因,我们或许应该首先了解一下水分子。
- Droplets or ice crystals are small enough to remain suspended aloft indefinitely. 水珠或冰晶非常小，以至于能够一直悬浮在高空中。
- As the cloud extends further upward, ice crystals may form because of low temperature there. 达到高空时温度会很低,冰粒也会在云中形成。
- Ice crystals begin to deform measurably under a unidirectional pressure of slightly less than one atmosphere. 在略小于一个单向大气压的压力下，冰晶就产生某种程度的变形。
