ice-albedo的意思|示意
冰反照率
ice-albedo的网络常见释义
反射 ...短卫壑啐题吉艘甏蹒挫蛙以荩摹湍蜥楠共肯砣莶套巯像庑梧柁拖焓钭芘镀篇诣彤伧珩蒂吼辏蛭蟓油麂砼缯敢 (b) 冰疛反射(ice-albedo)：冰疛反射作用是 另一个札回馈机制，下图说明明这个机制， 当地球变冷，南匇级疛冰被陎积增加，地表 比之前反射更多日光，减少了...
ice-albedo相关短语
1、 ice-albedo feedback 冰反照率反馈
ice-albedo相关例句
Sea ice retreat and snow melt reduce Earth's albedo, which can lead to increased warmth and further melting.
海冰的消退以及冰雪的融化降低了地球的反照率，这将导致温度继续增高冰雪继续消融。
A similar example of lowered albedo occurs when sea-ice melts and disappears, causing the darker coloured sea underneath to absorb more heat.
当海冰融化消失时，会同样降低反射率，导致深色的海底吸收更多的热量。
The scientists say this pattern is consistent with a climate process known as the ice-albedo feedback.
科学家认为这种模式，与被称为冰反射率回馈（ ice-albedo feedback）的气候变化过程的原理一致。
Transmission of Solar Radiation by Clouds over Snow and Ice Surfaces: a Parameterization in Terms of Optical Depth, Solar Zenith Angle, and Surface Albedo.
云和冰地表云对太阳辐射的传输：用光学厚度，太阳高度角和地表反照率参数化。
Part of this change is down to the albedo effect, with white, reflective ice replaced by dark water, which absorbs more of the sun's heat.
这种变化趋势的发生部分是因为黑色的水与白色的冰相比，反射效应低，从而吸收了更多来自太阳的热量。
This feedback loop, which is often referred to as the ice - albedo feedback, also delays the formation of new sea ice in autumn because of the accompanying surplus in oceanic heat storage.
这种反馈循环通常被称作“冰反射反馈”，它的伴随效应——海洋储热的过剩，常延迟秋季里新海冰的形成。