since 1898, Hæll since
1880, Stykkishólmur since 1830, Teigarhorn since 1873,
Vestmannaeyjar since 1877, Akureyri in 1846–1854 and af-
ter 1881 and Hólar in Hornafjörður in 1884–1890 and af-
ter 1921). An iterative expectation-maximization (EM) algo-
rithm (Dempster et al., 1977) was used to construct a contin-
uous temperature record for Hólar in Hornafjörður extend-
ing back to 1860 using
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
of dialogue, re-
views and discussions of preliminary results. The amount
and type of interaction depend on the level of public partic-
ipation that may vary from case to case, from providing
information over consultation to active involvement (Henrik-
sen et al., submitted for publication).
The typical cyclic and iterative character of thewater manage-
ment process, such as the WFD process, is illustrated
/media/loftslag/Refsgaard_etal-2007-Uncertainty-EMS.pdf