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Page 1: The effect of rainfall event sequencing on erosionesdac.jrc.ec.europa.eu/public_path/shared_folder/doc_pub/erosion... · The effect of rainfall event sequencing on erosion ... Repeated

The effect of rainfall event sequencing on erosion

Jantiene EM BaartmanAJAM Temme, A Veldkamp, VG Jetten, JM Schoorl

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Introduction & Objective

Extreme rainfall events contribute disproportionally to total erosion The timing of these events seems to be of importance Climate change predictions (Mediterranean)

● Less total rainfall; but● More intense events

Evaluate the effect of rainfall sequencing on long-term (centennial) erosion

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Methods

Methods: LAPSUS landscape evolution model

● Long-term redistribution of sediment

Study area: Prado, SE Spain• ~50 km2

• 435 – 1150 m.a.s.l.• Semi-arid: 250-530 mm/y• High inter-annual variation

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Methods

Rainfall data: 1997 – 2006; 9-yr record Repeated 11x to get a 99-yr rainfall timeseries Vary the order of occurrence of rainfall:

• 1997-2006 record repeated 11x• Order of years changed randomly, keeping total rainfall and

frequency the same (50 simulations)• Minimum scenario: 11x lowest year; 11x one-but-lowest year; etc• Maximum scenario: 11x highest year; 11x one-but-highest year; etc

Note: total P is equal in all runs!

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Results & Discussion

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Results & Discussion

Event sequencing: no linear relation between (high or low) rainfall and (high or low) net erosion

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Results & Discussion

Event sequencing: no linear relation between (high or low) rainfall and (high or low) net erosion

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Conclusions & Outlook

Non-linear behaviour is evident: ● Non-varying, average annual rainfall as input results

in peaks in simulated net erosion ● Variability in rainfall as input does not necessarily lead

to a corresponding peak in simulated erosion and peaks occur at points in time when no rainfall peak occurs.

What is the cause of this non-linear behaviour?● Change in connectivity?● Next step: analyse the spatial dynamics

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Thank you!

Based on:Baartman et al., 2013. Exploring the role of rainfall variability and extreme events in long-term landscape development. Catena 109: 25-38.

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Input: effective rainfall

Peff = P that becomes overland flow Determined based on LISEM simulated hydrographs and

Q/P ratios

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More extreme events

Inclusion of more extreme events• 10x erosivity of the most extreme event of the 1997-2006 record• Different frequencies of occurrence of such extreme event

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Increased erosivity

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Land use change scenario


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