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Journal ArticleDOI

Importance of rain evaporation and continental convection in the tropical water cycle

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TLDR
Measurements of the isotopic composition of water vapour near tropical clouds and over the tropical continents suggest that rainfall evaporation contributes significantly to lower troposphere humidity, and convection of vapour from both oceanic sources and evapotranspiration are the dominant moisture sources.
Abstract
Atmospheric moisture cycling is an important aspect of the Earth's climate system, yet the processes determining atmospheric humidity are poorly understood. For example, direct evaporation of rain contributes significantly to the heat and moisture budgets of clouds, but few observations of these processes are available. Similarly, the relative contributions to atmospheric moisture over land from local evaporation and humidity from oceanic sources are uncertain. Lighter isotopes of water vapour preferentially evaporate whereas heavier isotopes preferentially condense and the isotopic composition of ocean water is known. Here we use this information combined with global measurements of the isotopic composition of tropospheric water vapour from the Tropospheric Emission Spectrometer (TES) aboard the Aura spacecraft, to investigate aspects of the atmospheric hydrological cycle that are not well constrained by observations of precipitation or atmospheric vapour content. Our measurements of the isotopic composition of water vapour near tropical clouds suggest that rainfall evaporation contributes significantly to lower troposphere humidity, with typically 20% and up to 50% of rainfall evaporating near convective clouds. Over the tropical continents the isotopic signature of tropospheric water vapour differs significantly from that of precipitation, suggesting that convection of vapour from both oceanic sources and evapotranspiration are the dominant moisture sources. Our measurements allow an assessment of the intensity of the present hydrological cycle and will help identify any future changes as they occur.

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Citations
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Journal ArticleDOI

Widening of the tropical belt in a changing climate

TL;DR: The tropical belt has been widening over past decades, shifting the dry subtropical climate zones polewards around the world as discussed by the authors, and the observed recent rate of expansion is greater than climate model projections of expansion over the twenty-first century, suggesting that there is still much to be learned about this aspect of global climate change.
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Origin and fate of atmospheric moisture over continents

TL;DR: In this article, the authors make use of new definitions of moisture recycling to study the complete process of continental moisture feedback and identify regions that rely heavily on recycled moisture as well as those that are supplying the moisture.
Journal ArticleDOI

A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: Observations and simulations

TL;DR: In this article, the authors established a database of precipitation δ18O and used different models to evaluate the climatic controls of precipitation over the Tibetan Plateau (TP), revealing three distinct domains associated with the influence of the westerlies (northern TP), Indian monsoon (southern TP), and transition in between.
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Organic residue analysis in archaeology: the archaeological biomarker revolution*

Richard P. Evershed
- 01 Dec 2008 - 
TL;DR: Organic residue analysis utilizes analytical organic chemical techniques to identify the nature and origins of organic remains that cannot be characterized using traditional techniques of archaeological investigation (because they are either amorphous or invisible).
Journal ArticleDOI

Nuclear Quantum Effects in Water and Aqueous Systems: Experiment, Theory, and Current Challenges

TL;DR: The latest major developments in simulation algorithms and theory that have enabled the efficient inclusion of nuclear quantum effects in molecular simulations, permitting their combination with on-the-fly evaluation of the potential energy surface using electronic structure theory are reviewed.
References
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Journal ArticleDOI

Stable isotopes in precipitation

TL;DR: In this paper, the isotopic fractionation of water in simple condensation-evaporation processes is considered quantitatively on the basis of the fractionation factors given in section 1.2.
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The Changing Character of Precipitation

TL;DR: In this article, precipitation intensity, duration, frequency, and phase are as much of concern as total amounts, as these factors determine the disposition of precipitation once it hits the ground and how much runs off.
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Interaction of a Cumulus Cloud Ensemble with the Large-Scale Environment, Part I

TL;DR: In this paper, large-scale modification of the environment by cumulus clouds is discussed in terms of entrainment, detraining, evaporation, and subsidence, and budget equations for mass, static energy, water vapor, and liquid water are considered.
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Oxygen and hydrogen isotopes in the hydrologic cycle

TL;DR: In this article, the isotope fractionations that accompany the evaporation from the ocean and other surface waters and the reverse process of rain formation account for the most notable changes.
Journal ArticleDOI

The cause of decreased pan evaporation over the past 50 years.

TL;DR: In this article, the authors show that the decrease in evaporation is consistent with what one would expect from the observed large and widespread decreases in sunlight resulting from increasing cloud coverage and aerosol concentration.
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