Skip to main content

Research Repository

Advanced Search

All Outputs (3)

The effect of sampling effort on estimates of methane ebullition from peat (2017)
Journal Article
Ramirez, J. A., Baird, A. J., & Coulthard, T. J. (2017). The effect of sampling effort on estimates of methane ebullition from peat. Water Resources Research, 53(5), 4158-4168. https://doi.org/10.1002/2017wr020428

© 2017. American Geophysical Union. All Rights Reserved. We investigated the effect of sample size and sampling duration on methane bubble flux (ebullition) estimates from peat using a computer model. A field scale (10 m), seasonal ( > 100 days) simu... Read More about The effect of sampling effort on estimates of methane ebullition from peat.

Integrating the LISFLOOD-FP 2D hydrodynamic model with the CAESAR model: implications for modelling landscape evolution (2013)
Journal Article
Coulthard, T. J., Neal, J. C., Bates, P. D., Ramirez, J., de Almeida, G. A., & Hancock, G. R. (2013). Integrating the LISFLOOD-FP 2D hydrodynamic model with the CAESAR model: implications for modelling landscape evolution. Earth surface processes and landforms : the journal of the British Geomorphological Research Group, 38(15), 1897-1906. https://doi.org/10.1002/esp.3478

Landscape evolution models (LEMs) simulate the geomorphic development of river basins over long time periods and large space scales (100s-1000s of years, 100s of km2). Due to these scales they have been developed with simple steady flow models that e... Read More about Integrating the LISFLOOD-FP 2D hydrodynamic model with the CAESAR model: implications for modelling landscape evolution.

Vertical density gradient in the eastern North Atlantic during the last 30,000 years (2011)
Journal Article
Rogerson, M., Bigg, G. R., Rohling, E. J., & Ramirez, J. (2012). Vertical density gradient in the eastern North Atlantic during the last 30,000 years. Climate Dynamics, 39(3-4), 589-598. https://doi.org/10.1007/s00382-011-1148-4

Past changes in the density and momentum structure of oceanic circulation are an important aspect of changes in the Atlantic Meridional Overturning Circulation and consequently climate. However, very little is known about past changes in the vertical... Read More about Vertical density gradient in the eastern North Atlantic during the last 30,000 years.