关于海冰热传导的数学理论,包括盐水运动,发表在《皇家协会A议事录》上,可以改善极地地区的气候预测。 Mathematical theory on sea ice's thermal conductivity, incorporating brine movement, published in Proceedings of the Royal Society A, may improve climate predictions for polar regions.
《皇家协会A集》中的新数学理论侧重于海冰的热传导,这是气候模型中的一个关键参数。 A new mathematical theory in the Proceedings of the Royal Society A focuses on sea ice's thermal conductivity, a key parameter in climate models. 这项研究以早先的研究为基础,纳入了海冰内液体盐的流动,这可能会增加海水的热传输。 The study builds on earlier research, incorporating the movement of liquid brine within sea ice, which may increase its heat transport. 这一理论可以增进了解海冰对全球气候的影响,提高气候预测的准确性,特别是对极地区域的预测。 This theory could enhance understanding of sea ice's impact on global climate and improve the accuracy of climate predictions, particularly for polar regions.