At a time of unprecedented global change it is essential to distinguish short-term and local scale variability ("noise") from the low-amplitude longer wavelength signal of climate-driven change. Moreover, global responses to climate need to be separated from regional and local scale impacts and their interactions better understood to enable effective management of marine ecosystems. In this short editorial, we make the case for sustaining long-term and broad-scale observations of the oceans and coastal waters. First we consider the value of longterm observations drawing on work in the Western English Channel [1,2]; before considering the challenges of sustaining time series and cautioning that such observations are at risk in any period of financial constraints for public sector research funding. We conclude by discussing their relevance to policy and marine management. This editorial is written primarily from an ecological and inshore perspective reflecting the experience of the lead author but the general issues discussed apply equally to work in the open ocean.
Value of Long-Term and Broadside ObservationsEmpirical observations of the physics, chemistry and biology of the oceans and coastal seas have been made since the last quarter of the 19 th Century, given impetus by the major oceanographic expeditions (e.g. Porcupine -1868-1869, Challenger -1872-1876, Hirondelle I and II -1886-1922, Princesse Alice I and II -1886-1922, National -1889 and Valdivia -1898-1899 was an early and important attempt to integrate and network the efforts of multiple nations. In the UK the Marine Biological Association of the United Kingdom (MBA) led the work from its Laboratories at Lowestoft and Plymouth. The work in the English Channel initiated a long-running, but much interrupted time-series. Wars, funding cuts, institutional re-organisation and changes in research priorities all took their toll at various times over the last century.The Plymouth time-series (initially led by the MBA until 1987, with additional parameters measured by Plymouth Marine Laboratory (PML) , consolidated as the Western Channel Observatory www.westernchannelobservatory.org.uk in 2007, has made some major contributions to marine science over the last 100 years. One of the strengths of the Western English Channel time-series is its comprehensive nature covering physical, chemical measurements and observations of various biological compartments (phytoplankton, zooplankton, fish, benthos, intertidal assemblages) [1-6] of the ecosystem and its grid nature with two to three main stations E1, L5, L4 [2] on an inshore-offshore axis with both stratified and mixed water bodies. Observations in the Western English Channel have shown how climate fluctuations can drive whole nearshore and coastal ecosystems [3,4,[7][8][9][10]. These were apparent long before the recent spell of rapid warming since the late 1980s [1,2] and were coined "the Russell Cycle" by Cushing and Dickson [11]. Thus they provide a true fluctuating baseline of colder (early part of 20 th Cen...