Håkan Grudd



  • Statistical framework for evaluation of climate model simulations by use of climate proxy data from the last millennium-Part 3: Practical considerations, relaxed assumptions, and using tree-ring data to address the amplitude of solar forcing DOI: 10.5194/cp-11-425-2015
  • Drought-induced weakening of growth-temperature associations in high-elevation Iberian pines DOI: 10.1016/j.gloplacha.2014.11.011
  • Sulfur and iron accumulation in three marine-archaeological shipwrecks in the Baltic Sea: The Ghost, the Crown and the Sword DOI: 10.1038/srep04222
  • Spatial variability and temporal trends in water-use efficiency of European forests DOI: 10.1111/gcb.12717
  • Relationship between wood anatomy, tree-ring widths and wood density of Pinus sylvestris L. and climate at high latitudes in northern Sweden DOI: 10.1016/j.dendro.2014.07.003
  • Dendrochemical patterns of calcium, zinc, and potassium related to internal factors detected by energy dispersive X-ray fluorescence (EDXRF) DOI: 10.1016/j.chemosphere.2013.08.017
  • Stable carbon isotopes from Torneträsk, northern Sweden provide a millennial length reconstruction of summer sunshine and its relationship to Arctic circulation DOI: 10.1016/j.quascirev.2012.11.014
  • Potential bias in 'updating' tree-ring chronologies using regional curve standardisation: Re-processing 1500 years of Torneträsk density and ring-width data DOI: 10.1177/0959683612460791
  • Cool North European summers and possible links to explosive volcanic eruptions DOI: 10.1002/jgrd.50513
  • Advances towards improved low-frequency tree-ring reconstructions, using an updated Pinus sylvestris L. MXD network from the Scandinavian Mountains DOI: 10.1007/s00704-012-0787-7
  • A 1200-year multiproxy record of tree growth and summer temperature at the northern pine forest limit of Europe DOI: 10.1177/0959683612467483
  • Tree rings and volcanic cooling DOI: 10.1038/ngeo1645
  • Dendrochemistry of multiple releases of chlorinated solvents at a former industrial site DOI: 10.1021/es300318v
  • Common temperature signal in four well-replicated tree growth series from northern Fennoscandia DOI: 10.1002/jqs.2575
  • Cloud response to summer temperatures in Fennoscandia over the last thousand years DOI: 10.1029/2010GL046216
  • Blue intensity in Pinus sylvestris tree rings: A manual for a new palaeoclimate proxy DOI: 10.3959/2010-13.1
  • A critical evaluation of multi-proxy dendroclimatology in northern Finland DOI: 10.1002/jqs.1408
  • Dendroclimatology in Fennoscandia - from past accomplishments to future potential DOI: 10.5194/cp-6-93-2010
  • Spatial and temporal stability of the climatic signal in northern Fennoscandian pine tree-ring width and maximum density DOI: 10.1111/j.1502-3885.2008.00046.x
  • Trends in recent temperature and radial tree growth spanning 2000 years across northwest Eurasia DOI: 10.1098/rstb.2007.2199
  • Torneträsk tree-ring width and density ad 500-2004: A test of climatic sensitivity and a new 1500-year reconstruction of north Fennoscandian summers DOI: 10.1007/s00382-007-0358-2
  • New ice core evidence for a volcanic cause of the AD 536 dust veil DOI: 10.1029/2007GL032450
  • Long-term summer temperature variations in the Pyrenees DOI: 10.1007/s00382-008-0390-x
  • Blue intensity in Pinus sylvestris tree-rings: developing a new palaeoclimate proxy DOI: 10.1177/0959683607080523
  • Applied dendroecology and environmental forensics. Characterizing and age dating environmental releases: Fundamentals and case studies DOI: 10.1080/15275920601180487
  • Peatland pines as climate indicators? A regional comparison of the climatic influence on Scots pine growth in Sweden DOI: 10.1139/x02-071
  • A 7400-year tree-ring chronology in northern Swedish Lapland: Natural climatic variability expressed on annual to millennial timescales DOI: 10.1191/0959683602hl578rp
  • Climate variability 50,000 years ago in mid-latitude Chile as reconstructed from tree rings DOI: 10.1038/35069040
  • Swedish tree rings provide new evidence in support of a major, widespread environmental disruption in 1628 BC DOI: 10.1029/1999GL010852
  • Trees tell of past climates: but are they speaking less clearly today? DOI: 10.1098/rstb.1998.0191
  • Fifty years of mass balance and glacier front observations at the Tarfala research station EID: 2-s2.0-0030411206
  • Air temperature at Tarfala Research Station 1946-1995. DOI: 10.2307/520973
  • Small glaciers as sensitive indicators of climatic fluctuations EID: 2-s2.0-0025244844