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Tropical Montane Cloud and Rainforests

Derek Eamus, ALFREDO R. HUETE, Qiang Yu

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Abstract

Introduction Tropical montane cloud and rainforests are forests that occur at high elevation in tropical regions. They differ from tropical lowland forests because they experience low temperatures and because extensive mist and cloud cover alter the water and light environments compared to lowland forests. This chapter discusses the structure and behaviour of tropical montane forests (Fig. 18.1) and briefly compares these to lowland tropical forest. Due to their terrain and relative isolation, tropical montane forests have not received the same level of intense ecophysiological, modelling, or remote sensing, study that lowland forests have received, although this is slowly changing. Consequently the majority of studies have been leaf- and tree-scale and field-based. Eddy covariance methods have not been routinely applied to-date but developments in using remote sensing techniques with corrections for the influence of altitude, aspect and slope are occurring. Light, nutrient and temperature effects have major impacts on the ecophysiology, productivity and structure of tropical montane forests. Foliar uptake of water makes a significant contribution to the water status of the canopy. The questions addressed in this chapter include the following: Where do tropical montane forests occur? What leaf- and canopy-scale adaptations occur that allow montane forests to grow at altitude? Does photosynthetic capacity vary with altitude and what are the patterns in ET and productivity in these forests? Finally, this chapter addresses the question: do mist and clouds supply water directly to the canopy through foliar uptake? Types of Tropical Montane Cloud and Rainforests The case study of Amazonian rainforest (Chapter 17) focuses on seasonality of rainfall, phenological patterns and the impacts of drought on Amazonian rainforest productivity. That chapter examined the environmental controls of productivity in lowland tropical rainforest. In contrast, this case study examines tropical montane cloud and rainforest where the controls of productivity are generally temperature, light availability and sometimes, soil nutrient supply. Tropical montane cloud and rainforests occur at elevation in the tropics and are characterised as being shrouded in fog/cloud for a large fraction of the year. They have very large levels of endemism, very high levels of species richness, and are the source of large volumes of high quality drinking water for lower elevation sites. Cloud forests may increase the water yield of high altitude catchments through canopy interception and capture of cloud/fog water and through the suppression of evapotranspiration that occurs because of the presence of cloud/fog.

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Introduction Tropical montane cloud and rainforests are forests that occur at high elevation in tropical regions. They differ from tropical lowland forests because they experience low temperatures and because extensive mist and cloud cover alter the water and light environments compared to lowland forests. This chapter discusses the structure and behaviour of tropical montane forests (Fig. 18.1) and briefly compares these to lowland tropical forest. Due to their terrain and relative isolation, tropical montane forests have not received the same level of intense ecophysiological, modelling, or remote sensing, study that lowland forests have received, although this is slowly changing. Consequently the majority of studies have been leaf- and tree-scale and field-based. Eddy covariance methods have not been routinely applied to-date but developments in using remote sensing techniques with corrections for the influence of altitude, aspect and slope are occurring. Light, nutrient and temperature effects have major impacts on the ecophysiology, productivity and structure of tropical montane forests. Foliar uptake of water makes a significant contribution to the water status of the canopy. The questions addressed in this chapter include the following: Where do tropical montane forests occur? What leaf- and canopy-scale adaptations occur that allow montane forests to grow at altitude? Does photosynthetic capacity vary with altitude and what are the patterns in ET and productivity in these forests? Finally, this chapter addresses the question: do mist and clouds supply water directly to the canopy through foliar uptake? Types of Tropical Montane Cloud and Rainforests The case study of Amazonian rainforest (Chapter 17) focuses on seasonality of rainfall, phenological patterns and the impacts of drought on Amazonian rainforest productivity. That chapter examined the environmental controls of productivity in lowland tropical rainforest. In contrast, this case study examines tropical montane cloud and rainforest where the controls of productivity are generally temperature, light availability and sometimes, soil nutrient supply. Tropical montane cloud and rainforests occur at elevation in the tropics and are characterised as being shrouded in fog/cloud for a large fraction of the year. They have very large levels of endemism, very high levels of species richness, and are the source of large volumes of high quality drinking water for lower elevation sites. Cloud forests may increase the water yield of high altitude catchments through canopy interception and capture of cloud/fog water and through the suppression of evapotranspiration that occurs because of the presence of cloud/fog.

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Available abstract

Introduction Tropical montane cloud and rainforests are forests that occur at high elevation in tropical regions. They differ from tropical lowland forests because they experience low temperatures and because extensive mist and cloud cover alter the water and light environments compared to lowland forests. This chapter discusses the structure and behaviour of tropical montane forests (Fig. 18.1) and briefly compares these to lowland tropical forest. Due to their terrain and relative isolation, tropical montane forests have not received the same level of intense ecophysiological, modelling, or remote sensing, study that lowland forests have received, although this is slowly changing. Consequently the majority of studies have been leaf- and tree-scale and field-based. Eddy covariance methods have not been routinely applied to-date but developments in using remote sensing techniques with corrections for the influence of altitude, aspect and slope are occurring. Light, nutrient and temperature effects have major impacts on the ecophysiology, productivity and structure of tropical montane forests. Foliar uptake of water makes a significant contribution to the water status of the canopy. The questions addressed in this chapter include the following: Where do tropical montane forests occur? What leaf- and canopy-scale adaptations occur that allow montane forests to grow at altitude? Does photosynthetic capacity vary with altitude and what are the patterns in ET and productivity in these forests? Finally, this chapter addresses the question: do mist and clouds supply water directly to the canopy through foliar uptake? Types of Tropical Montane Cloud and Rainforests The case study of Amazonian rainforest (Chapter 17) focuses on seasonality of rainfall, phenological patterns and the impacts of drought on Amazonian rainforest productivity. That chapter examined the environmental controls of productivity in lowland tropical rainforest. In contrast, this case study examines tropical montane cloud and rainforest where the controls of productivity are generally temperature, light availability and sometimes, soil nutrient supply. Tropical montane cloud and rainforests occur at elevation in the tropics and are characterised as being shrouded in fog/cloud for a large fraction of the year. They have very large levels of endemism, very high levels of species richness, and are the source of large volumes of high quality drinking water for lower elevation sites. Cloud forests may increase the water yield of high altitude catchments through canopy interception and capture of cloud/fog water and through the suppression of evapotranspiration that occurs because of the presence of cloud/fog.

Key concepts: Rainforest, Cloud forest, Montane ecology, Tropical rainforest, Tropical forest, Tropical rain forest, Tropical and subtropical moist broadleaf forests, Geography

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