This
page compares weather observations made on the Hecla with recent
expected values (1961-90 normals). Although observations were made of
many meteorological variables, limitations in the data that were published and digitised means that only sea and air temperatures are available for analysis. It is
also possible to infer the sea-ice cover the ship experienced and
compare that to recent expected values. Both observed and comparative
recent values depend both on the date (position in the seasonal cycle)
and the position of the ship - here we show time-series comparisons
comparing the actual observations with those which would be expected by
a hypothetical ship following the same course, at the same time of
year, in recent decades.
Sea temperatureObserved (red dots) and modern equivalent (black line) sea-surface temperatures. The lower graph shows the range in expected sea-ice coverage - max and min values from HadISST for 1961-90.
Air TemperatureObserved (red dots) and modern equivalent (black line) air temperatures. The lower graph shows the range in expected sea-ice coverage - max and min values from HadISST for 1961-90.
Sea-IceThe
meteorological logs contain no explicit information on the sea-ice
cover, but it is possible to make inferences about the state of the
sea-ice from the information available. Sea-ice slows the ship down, it
is associated with low sea and air temperatures, and complete sea-ice
cover increases the air temperature variability (see AT graph above) -
effectively switching from a marine to a continental climate. From each
of these sources we can make an estimate of the sea ice cover: as proxy
observations they are likely to be imprecise, but collectively they
give a reasonable indication of the likely state of the ice coverage. Estimates of local sea-ice coverage from three different proxies (coloured points) and the range in expected recent sea-ice coverage - max and min values from HadISST for 1961-90. |