Groundwater flow estimation using temperature-depth profiles in a complex environment and a changing climate
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Understanding vertical water flux is vital for effective groundwater management.

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Obtaining vertical flux estimates is challenging in highly modified environments.

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Fluxes estimated using new temperature method that accounts for land surface warming.

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Fluxes can be estimated from temperature data, where other commonly used methods fail.

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Analyses relate to the hydrosphere, lithosphere, atmosphere and anthroposphere.

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