The twentieth century was the wettest period in northern Pakistan over the past millennium
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A technical perspective in modern tree-ring research--how to overcome dendroecological and wood anatomical challengesA 3,500-year tree-ring record of annual precipitation on the northeastern Tibetan PlateauLong-term trends in nitrogen isotope composition and nitrogen concentration in brazilian rainforest trees suggest changes in nitrogen cyclePlague dynamics are driven by climate variation.Comparing the performance of different stomatal conductance models using modelled and measured plant carbon isotope ratios (δ(13) C): implications for assessing physiological forcing.Treeline advances along the Urals mountain range - driven by improved winter conditions?Uniform climate sensitivity in tree-ring stable isotopes across species and sites in a mid-latitude temperate forest.Sensitivity of proxies on non-linear interactions in the climate system.Plague: past, present, and futureRecent enhancement of central Pacific El Niño variability relative to last eight centuriesExamining the large-scale convergence of photosynthesis-weighted tree leaf temperatures through stable oxygen isotope analysis of multiple data sets.Regional scale high resolution δ18O prediction in precipitation using MODIS EVICellulose (delta)18O is an index of leaf-to-air vapor pressure difference (VPD) in tropical plants.The oxygen isotope enrichment of leaf-exported assimilates--does it always reflect lamina leaf water enrichment?UV-laser-based microscopic dissection of tree rings - a novel sampling tool for δ(13) C and δ(18) O studies.Stable isotopes in tree rings: towards a mechanistic understanding of isotope fractionation and mixing processes from the leaves to the wood.Leaf water oxygen isotope measurement by direct equilibration.Thousand-year-long Chinese time series reveals climatic forcing of decadal locust dynamicsAn increase in the biogenic aerosol concentration as a contributing factor to the recent wetting trend in Tibetan Plateau.Seep-carbonate lamination controlled by cyclic particle flux.An oxygen isotope chronometer for cellulose deposition: the successive leaves formed by tillers of a C4 perennial grass.Climate signals in tree-ring δ(18) O and δ(13) C from southeastern Tibet: insights from observations and forward modelling of intra- to interdecadal variability.Recent Wetting and Glacier Expansion in the Northwest Himalaya and Karakoram.Forest response to increasing typhoon activity on the Korean peninsula: evidence from oak tree-rings.Tightly bound soil water introduces isotopic memory effects on mobile and extractable soil water pools.Identifying drivers of leaf water and cellulose stable isotope enrichment in Eucalyptus in northern Australia.Evaluation of whole cell fixation methods for the analysis of nanoscale surface features of Yersinia pestis KIM.Himalayan glaciers experienced significant mass loss during later phases of little ice ageCharacterization of sulfur deposition over the period of industrialization in Japan using sulfur isotope ratio in Japanese cedar tree rings taken from stumps.The enigma of effective path length for (18) O enrichment in leaf water of conifers.Changes in seasonal snow water equivalent distribution in High Mountain Asia (1987 to 2009).Climate variability in the northern and southern Altai Mountains during the past 50 years.A new serial pooling method of shifted tree ring blocks to construct millennia long tree ring isotope chronologies with annual resolution.δ²H, δ¹³C and δ¹⁸O from whole wood, α-cellulose and lignin methoxyl groups in Pinus sylvestris: a multi-parameter approach.Climatically driven synchrony of gerbil populations allows large-scale plague outbreaks.High-resolution palaeoclimatology of the last millennium: a review of current status and future prospectsTemporal stability in bristlecone pine tree-ring stable oxygen isotope chronologies over the last two centuriesA 350 year drought reconstruction from Alpine tree ring stable isotopesSeasonal transfer of oxygen isotopes from precipitation and soil to the tree ring: source water versus needle water enrichmentWet climate during the ‘Little Ice Age’ in the arid Tarim Basin, northwestern China
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The twentieth century was the wettest period in northern Pakistan over the past millennium
description
article publié dans la revue scientifique Nature
@fr
scientific article published in Nature
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wetenschappelijk artikel
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наукова стаття, опублікована в Nature у квітні 2006
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The twentieth century was the ...... istan over the past millennium
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The twentieth century was the ...... istan over the past millennium
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The twentieth century was the ...... istan over the past millennium
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The twentieth century was the ...... istan over the past millennium
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The twentieth century was the ...... istan over the past millennium
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The twentieth century was the ...... istan over the past millennium
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The twentieth century was the ...... istan over the past millennium
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David C. Frank
Gerald H. Haug
Gerhard H. Schleser
Kerstin S. Treydte
Matthias Winiger
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P2888
P304
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10.1038/NATURE04743
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P577
2006-04-27T00:00:00Z
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P6179
1010949198