نتایج جستجو برای: three crest slopes 0

تعداد نتایج: 1803443  

2004
Matthew Suderman David R. Wood

We study straight-line drawings of graphs with few segments and few slopes. Optimal results are obtained for all trees. Tight bounds are obtained for outerplanar graphs, 2-trees, and planar 3-trees. We prove that every 3-connected plane graph on n vertices has a plane drawing with at most 5n/2 segments and at most 2n slopes. We prove that every cubic 3-connected plane graph has a plane drawing ...

Journal: :Nature 2003
D W Burbank A E Blythe J Putkonen B Pratt-Sitaula E Gabet M Oskin A Barros T P Ojha

The hypothesis that abrupt spatial gradients in erosion can cause high strain rates in active orogens has been supported by numerical models that couple erosional processes with lithospheric deformation via gravitational feedbacks. Most such models invoke a 'stream-power' rule, in which either increased discharge or steeper channel slopes cause higher erosion rates. Spatial variations in precip...

2010
Peter Molnar

Although geomorphic observations suggest that the Sierra Nevada has tilted so that the crest has risen 1–2 km since late Miocene time, deuterium and oxygen-18 isotope concentrations in Cenozoic geologic materials decrease eastward across California and Nevada similarly to those in modern, orographically induced precipitation, as if little change in Sierra Nevadan elevations has occurred since E...

Journal: :American journal of physiology. Heart and circulatory physiology 2015
Noud van Helmond Blair D Johnson Timothy B Curry Andrew P Cap Victor A Convertino Michael J Joyner

We tested the hypothesis that markers of coagulation activation are greater during lower body negative pressure (LBNP) than those obtained during blood loss (BL). We assessed coagulation using both standard clinical tests and thrombelastography (TEG) in 12 men who performed a LBNP and BL protocol in a randomized order. LBNP consisted of 5-min stages at 0, -15, -30, and -45 mmHg of suction. BL i...

Journal: :Science 2016
M G A Lapotre R C Ewing M P Lamb W W Fischer J P Grotzinger D M Rubin K W Lewis M J Ballard M Day S Gupta S G Banham N T Bridges D J Des Marais A A Fraeman J A Grant K E Herkenhoff D W Ming M A Mischna M S Rice D Y Sumner A R Vasavada R A Yingst

Wind blowing over sand on Earth produces decimeter-wavelength ripples and hundred-meter- to kilometer-wavelength dunes: bedforms of two distinct size modes. Observations from the Mars Science Laboratory Curiosity rover and the Mars Reconnaissance Orbiter reveal that Mars hosts a third stable wind-driven bedform, with meter-scale wavelengths. These bedforms are spatially uniform in size and typi...

Journal: :Lung cancer 2017
Ben J Slotman Corinne Faivre-Finn Harm van Tinteren Astrid Keijser John Praag Joost Knegjens Matthew Hatton Iris van Dam Annija van der Leest Bart Reymen Jos Stigt Kate Haslett Devashish Tripathi Egbert F Smit Suresh Senan

INTRODUCTION In ES-SCLC patients with residual intrathoracic disease after first-line chemotherapy, the addition of thoracic radiotherapy reduces the risk of intrathoracic recurrence, and improves 2-year survival. To identify patient subgroups for future trials investigating higher dose (extra)thoracic radiotherapy, we investigated the prognostic importance of number and sites of metastases in ...

Journal: :Journal of international oral health : JIOH 2014
Deepak Bhorgonde K Nandakumar Punit R S Khurana V Santoshi Kumari M Sushendar Reddy Sabin Siddique

BACKGROUND In view of the importance of neutral zone in complete denture construction, it was thought feasible to determine the relation between the centre of the alveolar ridge crest in relation to the neutral zone in a buccolingual direction which will help in positioning of the teeth in a region of minimum conflict so that the stability of the denture is enhanced. MATERIALS & METHODS The p...

1997
I. Rychlik M. R. Leadbetter

In this paper, relationships between wave characteristics and upcrossing-and oscillation-intensities are used to construct conservative bounds for signiicant wave heights and amplitudes and for moments of waves crests and troughs. A concept of oscillation ltering is introduced for removing small waves. Results are illustrated by ve examples in which both Gaussian and non-Gaussian models for a s...

2000
G. Sauermann P. Rognon A. Poliakov

We present detailed shape measurements of several barchan dunes in southern Morocco, near Laayoune. Using these ˆ data, we disprove the concept of shape invariance of barchan dunes of different sizes. Nevertheless, some parts of the barchan dune scale and we try to distinguish these from non-scaling ones. Furthermore, we point out the importance of the exact position of the brink for the overal...

2016
M. G. A. Lapotre R. C. Ewing M. P. Lamb W. W. Fischer J. P. Grotzinger D. M. Rubin K. W. Lewis M. J. Ballard M. Day S. Gupta S. G. Banham N. T. Bridges D. J. Des Marais A. A. Fraeman J. A. Grant K. E. Herkenhoff D. W. Ming M. A. Mischna M. S. Rice D. A. Sumner A. R. Vasavada R. A. Yingst

Wind blowing over sand on Earth produces decimeter-wavelength ripples and hundred-meter– to kilometer-wavelength dunes: bedforms of two distinct size modes. Observations from the Mars Science Laboratory Curiosity rover and the Mars Reconnaissance Orbiter reveal that Mars hosts a third stable wind-driven bedform, with meter-scale wavelengths. These bedforms are spatially uniform in size and typi...

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