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Interactions between the atmosphere and terrestrial ecosystems: influence on weather and climate

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TLDR
In this article, the authors overview the short-term and long-term influences of the land surface on weather and climate, and conclude that terrestrial ecosystem dynamics on these timescales significantly influence atmospheric processes.
Abstract
This paper overviews the short-term (biophysical) and long-term (out to around 100 year timescales; biogeochemical and biogeographical) influences of the land surface on weather and climate. From our review of the literature, the evidence is convincing that terrestrial ecosystem dynamics on these timescales significantly influence atmospheric processes. In studies of past and possible future climate change, terrestrial ecosystem dynamics are as important as changes in atmospheric dynamics and composition, ocean circulation, ice sheet extent, and orbit perturbations.

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Investigating soil moisture-climate interactions in a changing climate: A review

TL;DR: In this paper, the authors provide a synthesis of past research on the role of soil moisture for the climate system, based both on modelling and observational studies, focusing on soil moisture-temperature and soil moistureprecipitation feedbacks, and their possible modifications with climate change.
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Climate change, phenology, and phenological control of vegetation feedbacks to the climate system

TL;DR: In this paper, the authors discuss the environmental drivers of phenology, and the impacts of climate change on phenology in different biomes, and assess the potential impact on these feedbacks of shifts in phenology driven by climate change.
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Hydrological functions of tropical forests: not seeing the soil for the trees?

TL;DR: In this article, a wide range of available scientific evidence with respect to the influence exerted by the presence or absence of a good forest cover on regional climate (rainfall), total and seasonal water yield (floods, low flows), as well as on different forms of erosion and catchment sediment yield under humid tropical conditions in general and in southeast Asia in particular.
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Water in a changing world

TL;DR: In this article, the authors conclude that over half of accessible fresh runoff globally is already appropriated for human use, and that more than 1 × 109 people currently lack access to clean drinking water and almost 3 ×109 people lack basic sanitation services, and because the human population will grow faster than increases in the amount of available fresh water, per capita availability of fresh water will decrease in the coming century.
References
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Book

An Introduction to Boundary Layer Meteorology

TL;DR: In this article, the boundary layer is defined as the boundary of a boundary layer, and the spectral gap is used to measure the spectral properties of the boundary layers of a turbulent flow.
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A Biochemical Model of Photosynthetic CO 2 Assimilation in Leaves of C 3 Species

TL;DR: Various aspects of the biochemistry of photosynthetic carbon assimilation in C3 plants are integrated into a form compatible with studies of gas exchange in leaves.
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Principles of Environmental Physics

TL;DR: In this paper, the second edition of the Second edition, the authors present a list of symbolic symbols for the field of environmental physical sciences, including the following: 1.GAS LAWS Pressure, volume and temperature Specific heats Lapse rate Water and water vapour Other gases 3. TRANSPORT LAWS General transfer equation Molecular transfer processes Diffusion coefficients Radiation laws 4. RADI ENVIRONMENT Solar radiation Terrestrial radiation Net radiation 5. MICROCLIMATOLOGY OF RADIATION (i) Interception Direct solar radiation Diffuse radiation Radiation in
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Analysis of factors controlling soil organic matter levels in Great Plains grasslands

TL;DR: In this article, a model of soil organic matter (SOM) quantity and composition was used to simulate steady-state organic matter levels for 24 grassland locations in the U.S. Great Plains.
Journal ArticleDOI

Carbon pools and flux of global forest ecosystems.

TL;DR: Slowing deforestation, combined with an increase in forestation and other management measures to improve forest ecosystem productivity, could conserve or sequester significant quantities of carbon.
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