POLAR OCEAN ECOSYSTEMS AND CHANGING CLIMATE

Using generalized linear models, we employed a model selection approach 18 to predict observed dis- tribution shifts resulting from (see Methods, Table 1) (i) the changes in

Figure 18 Four histograms from the Station Group “Transect” show the distribution of apical length measured for the species Fragilariopsis kerguelensis.. The Station Number and

resilience and explore possible futures and adapta- tion strategies. Into the model structure, indicators for the selected ecosystem services will be incorpo- rated. Focusing

Response of community mean cell size (calculated from mean total biovolumes divided by mean cell numbers for each mesocosm) to the experimental treatments, mesocosm 9 shown by an

Halliwell, G. 2015: OSSE impact analysis of airborne ocean surveys for improving upper-ocean dynamical and thermodynamical forecasts in the Gulf of Mexico. Baker, 2004: Estimation

In Chapter 1, we compile congruent findings of sea-ice thickness reduction from various observa- tion platforms, Chapter 2 discusses the impact of the decline of both extent

The El'gygytgyn lake region, Northeast Siberia, represents an ideal model system for studying the response of the methane cycle to climate change.. It is supposed to

The most important mis- matches (where >20% of cells assigned to one biome in the potential vegetation map were assigned to a different biome in the simulation) were between