Nordic Walking, modalidad terapéutica contra la fatiga relativa al cáncer

Existe evidencia de que el ejercicio físico puede mejorar los síntomas de los pacientes y supervivientes de cáncer y en especial la fatiga relativa al cáncer (FRC). El Nordic Walking (NW) es una novedosa forma de ejercicio físico que presenta ventajas fisiológicas y psicológicas significativas respecto de la marcha normal. Este artículo propone el NW como tratamiento terapéutico alternativo contra la FRC

Nordic Walking, modalidad terapéutica contra la fatiga relativa al cáncer

Existe evidencia de que el ejercicio físico puede mejorar los síntomas de los pacientes y supervivientes de cáncer y en especial la fatiga relativa al cáncer (FRC). El Nordic Walking (NW) es una novedosa forma de ejercicio físico que presenta ventajas fisiológicas y psicológicas significativas respecto de la marcha normal. Este artículo propone el NW como tratamiento terapéutico alternativo contra la FRC

Nordic Walking, modalidad terapéutica contra la fatiga relativa al cáncer

Existe evidencia de que el ejercicio físico puede mejorar los síntomas de los pacientes y supervivientes de cáncer y en especial la fatiga relativa al cáncer (FRC). El Nordic Walking (NW) es una novedosa forma de ejercicio físico que presenta ventajas fisiológicas y psicológicas significativas respecto de la marcha normal. Este artículo propone el NW como tratamiento terapéutico alternativo contra la FRC

Ice rafted debris in the Nordic Seas

A continuous 3.5 Myr IRD record was produced from Ocean Drilling Program (ODP) Site 907. A timescale based on magnetic polarity chrons, oxygen isotope stratigraphy (for the last 1Myr) and orbital tuning was developed. The record documents a stepwise inception of large-scale glacial cycles in the Nordic Seas region, the first being a marked expansion of the Greenland ice sheet at 3.3 Ma. A second step occurred at 2.74 Ma by an expansion of large scale ice sheets in the Northern Hemisphere. Ice sheet variability around the Nordic Seas was tightly coupled to global ice volume over the past 3.3 Myr. Between 3 and 1 Ma, most of the variance of the IRD signal is in the 41 kyr band, whereas the last 1 Myr is characterized by stronger 100 kyr variance. The Gamma Ray Porosity Evaluator (GRAPE) density record is closely linked with IRD variations and documents sub orbital variability resembling the late Quaternary Heinrich/Bond cycles.

Relative abundances of foraminifera and radiocarbon ages of selected cores obtained from the Nordic and Barents Sea

Ocean circulation changes along the continental shelf of the Nordic and Barents Seas have been investigated in order to reconstruct regional changes in the inflow of Atlantic Water (AW) through the last 16,000 calibrated (cal) years (yr) B.P. We have selected five time-slices representing the late glacial (16,000-15,000 cal yr B.P.), the Bølling-Allerød warm interstadials (14,500-13,500 cal yr B.P.), the Younger Dryas cold stadial (12,500-11,500 cal yr B.P.), the early Holocene (9500-7500 cal yr B.P.) and the late Holocene (4000-2000 cal yr B.P.). Twelve previously published records of the distribution of benthic foraminifera faunas and ice-rafted debris have been compiled. The earliest sign of Atlantic Water inflow was recorded at the northern Iceland shelf at 16,000-15,000 cal yr B.P. The inflow of warm AW to the Nordic Seas shelf has been persistent since, but with variable strength and geographic pattern. An apparent zonal seesaw pattern in the strength of the Norwegian Atlantic Current (NwAC) and the Irminger Current (IC) during the late glacial, Bølling-Allerød and Younger Dryas periods was found. During the Holocene, no zonal differences in the inflows of NwAC and IC were found. A strong meridional gradient with warmer conditions at lower latitudes and relatively cold conditions at high northern latitudes existed.

(Tables 1, 2) Permafrost borehole characteristics in the Nordic Area during the IPY 2007-2009

This paper provides a snapshot of the permafrost thermal state in the Nordic area obtained during the International Polar Year (IPY) 2007-2009. Several intensive research campaigns were undertaken within a variety of projects in the Nordic countries to obtain this snapshot. We demonstrate for Scandinavia that both lowland permafrost in palsas and peat plateaus, and large areas of permafrost in the mountains are at temperatures close to 0°C, which makes them sensitive to climatic changes. In Svalbard and northeast Greenland, and also in the highest parts of the mountains in the rest of the Nordic area, the permafrost is somewhat colder, but still only a few degrees below the freezing point. The observations presented from the network of boreholes, more than half of which were established during the IPY, provide an important baseline to assess how future predicted climatic changes may affect the permafrost thermal state in the Nordic area. Time series of active-layer thickness and permafrost temperature conditions in the Nordic area, which are generally only 10 years in length, show generally increasing active-layer depths and rising permafrost temperatures.