Matter and energy flow in Spitsbergen ornithogenic tundra

Investigations were carried out on matter and energy flow through ornithogenic Spitsbergen tundra (Hornsund area, Vestspitsbergen, Svalbard). Data are given on the inflow and dispersion of nutrients in tundra, vegetation, distribution and primary production, organic matter destruction, microfauna abundance and its classification into trophic groups, and the metabolic rate of the dominant species of microfauna. It was found that in the ecosystem examined herbivorous invertebrates are almost lacking, the dominant food chain is detritus type, and the majority of the plant matter produced is removed beyond the system to the sea, in the form of detritus. A qualitative model of matter cycling in the ecosystem is given.     

THE INFLUENCE OF GREENHOUSE WARMING ON THE ATMOSPHERIC COMPONENT OF THE HYDROLOGICAL CYCLE

An atmosphere–ocean climate box model is used to examine the influence of cloud feedback on the equilibria of the climate system. The model consists of three non-linear ordinary differential equations, which are simplified forms of the first law of thermodynamics for the atmosphere and ocean and the continuity equation for the atmospheric component of the hydrological cycle. The mass continuity equation expresses the cloud liquid water content as a function of the evaporation rate from the ocean surface and the precipitation rate. Cloud formation releases latent heat. The model clouds also absorb solar energy at a rate consistent with recent findings. The model simulates snow–ice albedo feedback, water vapour feedback and cloud feedback. The global mean precipitation and surface temperature are analysed as they respond to enhanced greenhouse warming. Model results show that cloud feedback can lead to the occurrence of multiple climate equilibria. Some of these are warmer than the present equilibrium, with increased precipitation, while others are colder, with reduced precipitation. If the cloud feedback is weak, enhanced greenhouse forcing leads to a small alteration of the present equilibrium. If the cloud feedback is strong enough, the climate system can be forced into a warmer and wetter equilibrium.