Freeze-thaw weathering is an important surface process and the complex underlying
processes can be understood as an interplay between rock properties and its dynamic …

We present a review of the changing state of European permafrost within a spatial zone that
includes the continuous high latitude arctic permafrost of Svalbard and the discontinuous …

Controlling dropwise condensation is fundamental to water-harvesting systems,,,
desalination, thermal power generation,,,,, air conditioning, distillation towers, and numerous …

Measuring the evolution of pore structures is the most straightforward approach to assessing
frost damage in porous rocks. Systematic and fine measurement of pore structures is critical …

Glaciers and Glaciation is the classic textbook for all students of glaciation. Stimulating and
accessible, it has established a reputation as a comprehensive and essential resource. In …

Petra, Angkor, Copan, Venice, Lascaux, Easter Island—all are examples of irreplaceable
cultural heritage built in stone and now slowly disappearing. In 1996 the Getty Conservation …

In this paper, we develop a mechanical model that relates the destabilization of thawing
permafrost rock slopes to temperature‐related effects on both, rock‐and ice‐mechanics; and …

Glaciation and deglaciation, along with their associated climatic and non-climatic processes,
modify slope stresses and influence slope stability. Paraglacial slope failures are those that …

The freeze–thaw action of water inside rocks' pores, cracks, and joints plays a dominant role
in physical rock weathering where the temperature fluctuates across 0° C. To understand …

Rockfall is one of the main geomorphological processes that affects the evolution and
stability of rock-walls. At high elevations, rockfall is largely climate-driven, very probably …