Add to ORKGBy using the micrometeorological observation data in a mossy area and the daily meteorological data of Great Wall Station (GWS) in the Antarctic, two microclimate features are revealed in this study. First, the amplitude of diurnal variation of temperature in the lower layer above the ground in the mossy area is decreasing rapidly with altitude under any kind of weather conditions; Second, the difference between the diurnal mean surface (0 cm height) temperature and mean surface air (150cm height) temperature in the mossy area is much smaller than in GWS. The aforesaid difference is probably due to the difference between the moss cushion in the microclimatic observation field and the bare sandy soil in GWS, that may have an important influe...
A CALM grid with a data logger system to monitor the active layer thermal regime was established on ...
Meteorological measurements were performed on the non-glaciated coastal area of the Ferraz Station, ...
Mosses are dominant components of high-latitude environments, and Signy Island (maritime Antarctic) ...
The microclimatic condition was observed by the specially prepared selfrecording ther-mistor instrum...
In the summer 2000-01, thermal monitoring of the permafrost active layer within various terrestrial ...
Temperatures within soil and plant habitats on Signy Island in the maritime Antarctic were measured ...
Ground surface temperature (GST) and active layer thickness (ALT) are key indicators of climate chan...
Climate change is now evident also in Antarctica, with impacts both on the abiotic and the biotic co...
An understanding of the microclimatology of the ice free areas in Antarctica is needed to better qua...
Climate change is now evident also in Antarctica, with impacts both on the abiotic and the biotic co...
In the summer 2000-01, thermal monitoring of the permafrost active layer within various terrestrial...
The temperature experienced by micro-invertebrates in extreme environments (such as those of Antarc...
A CALM grid with a data logger system to monitor the active layer thermal regime was established on ...
Meteorological measurements were performed on the non-glaciated coastal area of the Ferraz Station, ...
Mosses are dominant components of high-latitude environments, and Signy Island (maritime Antarctic) ...
The microclimatic condition was observed by the specially prepared selfrecording ther-mistor instrum...
In the summer 2000-01, thermal monitoring of the permafrost active layer within various terrestrial ...
Temperatures within soil and plant habitats on Signy Island in the maritime Antarctic were measured ...
Ground surface temperature (GST) and active layer thickness (ALT) are key indicators of climate chan...
Climate change is now evident also in Antarctica, with impacts both on the abiotic and the biotic co...
An understanding of the microclimatology of the ice free areas in Antarctica is needed to better qua...
Climate change is now evident also in Antarctica, with impacts both on the abiotic and the biotic co...
In the summer 2000-01, thermal monitoring of the permafrost active layer within various terrestrial...
The temperature experienced by micro-invertebrates in extreme environments (such as those of Antarc...
A CALM grid with a data logger system to monitor the active layer thermal regime was established on ...
Meteorological measurements were performed on the non-glaciated coastal area of the Ferraz Station, ...
Mosses are dominant components of high-latitude environments, and Signy Island (maritime Antarctic) ...