This work was broadened in 1998 using a network of over 300 tree - ring records
across high northern latitudes (Briffa 1998).
Not exact matches
The Arctic System Reanalysis (ASR), a
high - resolution regional assimilation of model output, observations, and satellite data
across the mid - and
high latitudes of the
Northern Hemisphere for the period 2000 — 2012 has been performed at 30 km (ASRv1) and 15 km (ASRv2) horizontal resolution using the polar version of the Weather Research and Forecasting (WRF) model and the WRF Data Assimilation (WRFDA) System.
Gesturing to an indelible deep green hue streaked
across the United States and Europe viewers were told, «in the
high latitudes of the
Northern hemisphere emissions were less than absorption levels.»
This showed that recovery took longest in the
high northern latitudes and in the tropics, regions where the climate system is already vulnerable, but that it was taking longer
across regions worldwide.
Diverging trends between tree - ring chronologies and temperature in the late twentieth century have been observed
across the
high latitudes of the
Northern Hemisphere (see D'Arrigo et al. 2007 and references therein).