HESS Opinions: Science in today's media landscape – challenges and lessons from hydrologists and journalists by Stefanie R. Lutz, Andrea Popp, Tim Van Emmerik, Tom Gleeson, Liz Kalaugher, Karsten Mobius, Tonie Mudde, Brett Walton, Rolf Hut, Hubert Savenije, Louise Slater, Anna Solcerova, Cathelijne Stoof, Matthias Zink

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Accurate power sharing of hybrid energy storage system in DC shipboard power system based on quadratic programming algorithm by Tianling Shi, Heyu Liu, Fei Wang, Shengqi Zhang, Hui Guo, Zhengyu Lin

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If erring is human, is system use divine? Omission errors during post-adoptive system use by Lazaros Goutas, Basil Hess, Juliana Sutanto

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Using variograms to detect and attribute hydrological change by Andrew Chiverton, Jamie Hannaford, Ian Holman, Ron Corstanje, Christel Prudhomme, Tim Hess, John P. Bloomfield

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Which catchment characteristics control the temporal dependence structure of daily river flows? by Andrew Chiverton, Jamie Hannaford, Ian Holman, Ron Corstanje, Christel Prudhomme, John P. Bloomfield, Tim Hess

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Climate change and water in the UK – past changes and future prospects by Glen Watts, Richard W. Battarbee, John P. Bloomfield, Jill Crossman, Andre Daccache, Isabelle Durance, J. Alex Elliott, Grace Garner, Jamie Hannaford, David M. Hannah, Tim Hess, Christopher R. Jackson, Alison L. Kay, Martin Kernan, Jerry Knox, Jonathan Mackay, Donald T. Monteith, Steve J. Ormerod, Jemima Rance, Marianne E. Stuart, Andrew J. Wade, Steven D. Wade, Keith Weatherhead, Paul G. Whitehead, Robert Wilby

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Dispersionless Hirota equations and the genus 3 hyperelliptic divisor by Fabien Clery, Evgeny Ferapontov

“…Here we prove that the generic 3D Hirota equation is given by the remarkable formula ϑm(τ ) = 0, τ = i Hess(u) where ϑm is any genus 3 theta constant with even characteristics and Hess(u) is the 3 × 3 Hessian matrix of a (real-valued) function u(x1, x2, x3). …”
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Macroinvertebrate data from sand, silt, gravel habitats in five English rivers by Kate Mathers, Patrick Armitage, Melanie Bickerton, Matthew Hill, Morwenna Mckenzie, Isabel Pardo, David Tickner, Paul Wood

“…Data were collected using either a 15-second kick sample (900 µm pond net) or via a cylinder sampler (comparable to a hess sampler) on the spot in three discrete substrate habitats (gravel, sand, silt). …”
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The relationship between depth and age in the North Pacific Ocean by John Hillier, A.B. Watts

“…Using a thermal conductivity, k, of 3.138 mW m−2 as previous studies, however, gives a plate of similar thickness (i.e., thermal thickness, L, of ∼115 km) but one which is unreasonably hot (i.e., temperature at the base of the plate, Tb, of 1522 °C) and inexpansive (i.e., coefficient of thermal expansion, α, of 2.57×10−5 °C−1). More reasonable values (i.e., Tb = 1363°C, k = 3.371 W m−1 °C−1, α = 2.77×10−5 °C−1, and L = 120 km) are obtained if the crustal thickness is used to constrain Tb and a certain amount of the surface heat flow is allowed to be radiogenically generated within the oceanic lithosphere.…”
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