Results 171 to 180 of about 2,403 (235)

Novel method for rubber hand illusion strength measurement based on inverse multidimensional scaling. [PDF]

Behav Res Methods
Litwin P, Kubik K, Longo MR.
europepmc   +1 more source

Automated determination of transport and depositional environments in sand and sandstones. [PDF]

Proc Natl Acad Sci U S A
Hasson M, Marvin MC, Lapôtre MGA.
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Underactive bladder, Fowler's syndrome are potentially curable by uterosacral ligament repair. [PDF]

Ann Transl Med
Wenk MJ, Bush M, Swash M, Liedl B, Witczak M.   +4 more
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The role of psychological flexibility in relation to health outcomes in people in remission from cancer. [PDF]

Br J Health Psychol
Al-Abbadey M, Tomescu-Stachie S, Kaklamanou D, Jarrett N, Merwood A, Tyndall I, McCracken L.   +6 more
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Understanding barriers and facilitators to palliative and end-of-life care research: a mixed method study of generalist and specialist health, social care, and research professionals. [PDF]

BMC Palliat Care
Walshe C, Dunleavy L, Preston N, Payne S, Ellershaw J, Taylor V, Mason S, Nwosu AC, Gadoud A, Board R, Swash B, Coyle S, Dickman A, Partridge A, Halvorsen J, Hulbert-Williams N.   +15 more
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Simultaneous ultrasound and needle electromyography recording of fasciculations in amyotrophic lateral sclerosis. [PDF]

Clin Neurophysiol Pract
Sugimoto T, Tachiyama K, Hironaka A, Naito H, Nakamori M, Aoki S, Yamazaki Y, Maruyama H.   +7 more
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Prediction of swash motion and run-up including the effects of swash interaction

Coastal Engineering, 2005
Modifications to a model describing swash motion based on solutions to the non-linear shallow water equations were made to account for interaction between up-rush and back-wash at the still water shoreline and within the swash zone. Inputs to the model are wave heights and arrival times at the still water shoreline.
Hans Hanson, Magnus Larson
exaly   +2 more sources

The swash zone

2020
This chapter describes the morphological features and key processes related to the swash zone, situated at the landward edge of the inundated part of the beach system. It is where incoming surf zone waves force oscillatory motion of the shoreline at a variety of frequencies.
Hughes, Michael G., Baldock, Tom E.
openaire   +3 more sources

Swash and swash mark

Eos, Transactions American Geophysical Union, 1951
The time interval between swashes was found to be longer for gentle marine beaches than for steep ones owing to differing effectiveness of the beaches as wave filters. This relationship offers a possible means of determining the angle of beach slope from aerial reconnaissance.
openaire   +1 more source