Reduced sensitivity of recent tree-growth to temperature at high northern latitudes

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Items 201–300 of 814

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44. Climatic significance of the marginalization of Scots pine (Pinus sylvestris L.)c. 2500 BC at White Moss, south Cheshire, UK
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45. Statistical and process‐based modeling analyses of tree growth response to climate in semi‐arid area of north central China: A case study of Pinus tabulaeformis
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46. Are multiproxy climate reconstructions robust?
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47. Dendroclimatology: extracting climate from trees
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48. Temperature changes on the Tibetan Plateau during the past 600 years inferred from ice cores and tree rings
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49. No divergence in Cassiope tetragona: persistence of growth response along a latitudinal temperature gradient and under multi-year experimental warming
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51. Divergent responses to climate factors in the radial growth of Larix sibirica in the eastern Tianshan Mountains, northwest China
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52. Radial growth of Larix sibirica was more sensitive to climate at low than high altitudes in the Altai Mountains, China
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56. Differences in the Climate-Growth Relationship of Scots Pine: A Case Study from Poland and Hungary
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57. On the spatiotemporal characteristics of Fennoscandian tree-ring based summer temperature reconstructions
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58. Tree-limit rise and recent warming: a geoecological case study from the Swedish Scandes
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63. Precipitation reconstruction for the southern Altay Mountains (China) from tree rings of Siberian spruce, reveals recent wetting trend
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65. Growth response of alpine treeline forests to a warmer and drier climate on the southeastern Tibetan Plateau
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66. Diurnal and seasonal changes in stem increment and water use by yellow poplar trees in response to environmental stress
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67. The future of high-elevation, five-needle white pines in Western North America: Proceedings of the High Five Symposium
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68. Twentieth century trends in tree ring stable isotopes (δ13C and δ18O) of Larix sibirica under dry conditions in the forest steppe in Siberia
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80. Unprecedented recent warming rate and temperature variability over the east Tibetan Plateau inferred from Alpine treeline dendrochronology
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83. A 352-year record of summer temperature reconstruction in the western Tianshan Mountains, China, as deduced from tree-ring density
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