Passive open-top devices have been proposed as a method to experimenta
lly increase temperature in high-latitude ecosystems. There is, howeve
r, little documentation on the efficacy of these devices. This paper e
xamines the performance of four open-top chambers for altering tempera
ture at six sites in the Arctic and Antarctica. Most of the heating ef
fect was due to daytime warming above ambient; occasional night-time c
ooling below ambient, especially of air temperatures, depressed mean d
aily temperature. The mean daily temperatures at four arctic sites wer
e generally increased by 1.2-1.8 degrees C; but occasionally, temperat
ure depressions also occurred. Under optimal conditions at the antarct
ic site (dry soils, no vegetation, high radiation) mean daily soil tem
peratures were increased by +2.2 degrees C (-10 cm) to +5.2 degrees C
(0 cm). Protection from wind may Flay a more important role than tempe
rature per se in providing a favourable environment for plant growth w
ithin open-top devices. Wind speed had a generally negative impact on
mean daily temperature. Daily global radiation was both positively and
negatively related to chamber temperature response. The effect of cha
mbers on snow accumulation was variable with the Alexandra Fjord site
showing an increased accumulation in chambers but no difference in the
date of snowmelt, while at Latnjajaure in a deep snowfall site, snowm
elt occurred 1-2 weeks earlier in chambers, potentially increasing the
growing season. Selection of a passive temperature-enhancing system r
equires balancing the temperature enhancement desired against potentia
l unwanted ecological effects such as chamber overheating and altered
light, moisture, and wind. In general, the more closed the temperature
-enhancing system, the higher is the temperature enhancement, but the
larger are the unwanted ecological effects. Open-top chambers alter te
mperature significantly and minimize most unwanted ecological effects;
as a consequence, these chambers are a useful tool for studying the r
esponse of high-latitude ecosystems to warming.