Importance of rain evaporation and continental convection in the tropical water cycle.
about
Vapor hydrogen and oxygen isotopes reflect water of combustion in the urban atmosphereWater, plants, and early human habitats in eastern AfricaAngiosperm leaf vein evolution was physiologically and environmentally transformativeMeasurements of water vapor isotope ratios with wavelength-scanned cavity ring-down spectroscopy technology: new insights and important caveats for deuterium excess measurements in tropical areas in comparison with isotope-ratio mass spectrometry.Regional scale high resolution δ18O prediction in precipitation using MODIS EVIDynamic processes governing lower-tropospheric HDO/H2O ratios as observed from space and ground.Unraveling quantum mechanical effects in water using isotopic fractionation.Rainforest-initiated wet season onset over the southern Amazon.Potential for natural evaporation as a reliable renewable energy resource.Hydrogen isotope correction for laser instrument measurement bias at low water vapor concentration using conventional isotope analyses: application to measurements from Mauna Loa Observatory, Hawaii.Evidence of a large cooling between 1690 and 1740 AD in southern Africa.Negative soil moisture-precipitation feedback in dry and wet regions.Efficient methods and practical guidelines for simulating isotope effects.Direct path integral estimators for isotope fractionation ratios.Stable isotopes in water vapor and rainwater over Indian sector of Southern Ocean and estimation of fraction of recycled moisture.Isotopic study of intraseasonal variations of plant transpiration: an alternative means to characterise the dry phases of monsoon.Poleward expansion of the tropical belt derived from upper tropospheric water vapourA method for estimating the contribution of evaporative vapor from Nam Co to local atmospheric vapor based on stable isotopes of water bodiesComparison of an isotopic atmospheric general circulation model with new quasi-global satellite measurements of water vapor isotopologuesUsing atmospheric trajectories to model the isotopic composition of rainfall in central KenyaDiagnosing Atmospheric Influences on the Interannual 18O/16O Variations in Western U.S. PrecipitationEmerging Technologies and Synergies for Airborne and Space-Based Measurements of Water Vapor ProfilesImportance of the Saharan heat low in controlling the North Atlantic free tropospheric humidity budget deduced from IASI <i>δ</i>D observationsFootprint of recycled water subsidies downwind of Lake MichiganStable water isotopes in the ECHAM5 general circulation model: Toward high-resolution isotope modeling on a global scaleControlling factors of rainwater and water vapor isotopes at Bangalore, India: Constraints from observations in 2013 Indian monsoonObservation system simulation experiments using water vapor isotope informationWater vapor δD dynamics over China derived from SCIAMACHY satellite measurementsA seasonality of δD of water vapor (850-500 hPa) observed from space over Jeju Island, KoreaInfluence of synoptic weather events on the isotopic composition of atmospheric moisture in a coastal city of the western United StatesInterannual variability of H218O in precipitation over the Asian monsoon regionThe cause of the seasonal variation in the oxygen isotopic composition of precipitation along the western U.S. coastProcess-evaluation of tropospheric humidity simulated by general circulation models using water vapor isotopic observations: 2. Using isotopic diagnostics to understand the mid and upper tropospheric moist bias in the tropics and subtropicsProcess-evaluation of tropospheric humidity simulated by general circulation models using water vapor isotopologues: 1. Comparison between models and observationsUnderstanding the Sahelian water budget through the isotopic composition of water vapor and precipitationEvaluating climate model performance in the tropics with retrievals of water isotopic composition from Aura TESIntraseasonal isotopic variation associated with the Madden-Julian OscillationAsian monsoon hydrometeorology from TES and SCIAMACHY water vapor isotope measurements and LMDZ simulations: Implications for speleothem climate record interpretationA meta-analysis of water vapor deuterium-excess in the midlatitude atmospheric surface layerTropical rain recycling
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P2860
Importance of rain evaporation and continental convection in the tropical water cycle.
description
2007 nî lūn-bûn
@nan
2007年の論文
@ja
2007年論文
@yue
2007年論文
@zh-hant
2007年論文
@zh-hk
2007年論文
@zh-mo
2007年論文
@zh-tw
2007年论文
@wuu
2007年论文
@zh
2007年论文
@zh-cn
name
Importance of rain evaporation and continental convection in the tropical water cycle.
@en
Importance of rain evaporation and continental convection in the tropical water cycle.
@nl
type
label
Importance of rain evaporation and continental convection in the tropical water cycle.
@en
Importance of rain evaporation and continental convection in the tropical water cycle.
@nl
prefLabel
Importance of rain evaporation and continental convection in the tropical water cycle.
@en
Importance of rain evaporation and continental convection in the tropical water cycle.
@nl
P2093
P356
P1433
P1476
Importance of rain evaporation and continental convection in the tropical water cycle.
@en
P2093
David Noone
John Worden
Kevin Bowman
Tropospheric Emission Spectrometer Science Team and Data contributors
P2888
P304
P356
10.1038/NATURE05508
P407
P577
2007-02-01T00:00:00Z
P5875
P6179
1026116863