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. A new annually resolved sedimentary record of SouthernHemisphere mid-latitude hydroclimate was recovered from Lake Ohau, SouthIsland, New Zealand, in March 2016. The Lake Ohau Climate History (LOCH)project acquired cores from two sites (LOCH-1 and -2) that preserve sequencesof laminated mud that accumulated since the lake formed ∼  17 000 yearsago. Cores were recovered using a purpose-built barge and drilling systemdesigned to recover soft sediment from thick sedimentary sequences in lakesystems up to 150 m deep. This system can be transported in two to three40 ft long shipping containers and is suitable for use in a range ofgeographic locations. A comprehensive suite of data has been collected fromthe sedimentary sequence using state-of-the-art analytical equipment andtechniques. These new observations of past environmental variability augmentthe historical instrumental record and are currently being integrated withregional climate and hydrological modelling studies to explore causes ofvariability in extreme/flood events over the past several millennia.

A high-resolution climate record spanning the past 17 000 years recovered from Lake Ohau, South Island, New Zealand