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Artículos de revistas sobre el tema "Tides"

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Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 31 de julio de 2024

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1

Ray, Richard D. y David E. Cartwright. "Times of peak astronomical tides". Geophysical Journal International 168, n.º 3 (marzo de 2007): 999–1004. http://dx.doi.org/10.1111/j.1365-246x.2006.03293.x.

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2

Cuthbert, Rebecca. "Tides Advance, Tides Retreat". American Book Review 42, n.º 3 (2021): 27–29. http://dx.doi.org/10.1353/abr.2021.0044.

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3

Agnew, Duncan C. "Time and tide: pendulum clocks and gravity tides". History of Geo- and Space Sciences 11, n.º 2 (16 de septiembre de 2020): 215–24. http://dx.doi.org/10.5194/hgss-11-215-2020.

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Abstract. Tidal fluctuations in gravity will affect the period of a pendulum and hence the timekeeping of any such clock that uses one. Since pendulum clocks were, until the 1940s, the best timekeepers available, there has been interest in seeing if tidal effects could be observed in the best performing examples of these clocks. The first such observation was in 1929, before gravity tides were measured with spring gravimeters; at the time of the second (1940–1943), such gravimeters were still being developed. Subsequent observations, having been made after pendulum clocks had ceased to be the best available timekeepers and after reliable gravimeter measurements of tides, have been more of an indication of clock quality than a contribution to our knowledge of tides. This paper describes the different measurements and revisits them in terms of our current knowledge of Earth tides. Doing so shows that clock-based systems, though noisier than spring gravimeters, were an early form of an absolute gravimeter that could indeed observe Earth tides.

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4

Houston, D. "Tides". English 48, n.º 192 (1 de septiembre de 1999): 200. http://dx.doi.org/10.1093/english/48.192.200a.

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5

Crew, E. W. "Tides". Electronics and Power 33, n.º 8 (1987): 491. http://dx.doi.org/10.1049/ep.1987.0304.

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6

Ojaide, Tanure y Isidore Okpewho. "Tides". World Literature Today 68, n.º 3 (1994): 621. http://dx.doi.org/10.2307/40150555.

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7

Hewitt, Paul. "TIDES". Physics Teacher 44, n.º 4 (abril de 2006): 205. http://dx.doi.org/10.1119/1.2186227.

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8

Nash, Jonathan D., Samuel M. Kelly, Emily L. Shroyer, James N. Moum y Timothy F. Duda. "The Unpredictable Nature of Internal Tides on Continental Shelves". Journal of Physical Oceanography 42, n.º 11 (1 de noviembre de 2012): 1981–2000. http://dx.doi.org/10.1175/jpo-d-12-028.1.

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Abstract Packets of nonlinear internal waves (NLIWs) in a small area of the Mid-Atlantic Bight were 10 times more energetic during a local neap tide than during the preceding spring tide. This counterintuitive result cannot be explained if the waves are generated near the shelf break by the local barotropic tide since changes in shelfbreak stratification explain only a small fraction of the variability in barotropic to baroclinic conversion. Instead, this study suggests that the occurrence of strong NLIWs was caused by the shoaling of distantly generated internal tides with amplitudes that are uncorrelated with the local spring-neap cycle. An extensive set of moored observations show that NLIWs are correlated with the internal tide but uncorrelated with barotropic tide. Using harmonic analysis of a 40-day record, this study associates steady-phase motions at the shelf break with waves generated by the local barotropic tide and variable-phase motions with the shoaling of distantly generated internal tides. The dual sources of internal tide energy (local or remote) mean that shelf internal tides and NLIWs will be predictable with a local model only if the locally generated internal tides are significantly stronger than shoaling internal tides. Since the depth-integrated internal tide energy in the open ocean can greatly exceed that on the shelf, it is likely that shoaling internal tides control the energetics on shelves that are directly exposed to the open ocean.

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9

Gemael, Camil. "Earth Tides in Brazil". Zentralblatt für Geologie und Paläontologie, Teil I 1985, n.º 9-10 (9 de julio de 1986): 1495–500. http://dx.doi.org/10.1127/zbl_geol_pal_1/1985/1986/1495.

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10

Kuppers, Petra. "13 Tides". Ecozon@: European Journal of Literature, Culture and Environment 12, n.º 1 (14 de febrero de 2021): 215–18. http://dx.doi.org/10.37536/ecozona.2021.12.1.3813.

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11

Perkins, Sid. "Toxic Tides". Science News 169, n.º 23 (10 de junio de 2006): 358. http://dx.doi.org/10.2307/4019240.

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12

Frater, D. A. "mourning tides". Annals of Internal Medicine 171, n.º 12 (17 de diciembre de 2019): 945. http://dx.doi.org/10.7326/m19-0931.

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13

&NA;. "Changing Tides". Critical Care Nursing Quarterly 33, n.º 2 (abril de 2010): 175–76. http://dx.doi.org/10.1097/cnq.0b013e3181d8fe5d.

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14

Race, Tara Kay y Janet Skees. "Changing Tides". Critical Care Nursing Quarterly 33, n.º 2 (abril de 2010): 163–74. http://dx.doi.org/10.1097/cnq.0b013e3181d91475.

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15

Anderson, Donald M. "Red Tides". Scientific American 271, n.º 2 (agosto de 1994): 62–68. http://dx.doi.org/10.1038/scientificamerican0894-62.

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16

Olson, Donald W. y Thomas E. Lytle. "High tides?" Physics Teacher 37, n.º 9 (diciembre de 1999): 517. http://dx.doi.org/10.1119/1.880387.

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17

Connell, Raewyn. "Global Tides". Social Currents 1, n.º 1 (febrero de 2014): 5–12. http://dx.doi.org/10.1177/2329496513513961.

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18

Kuo, John T. "Earth tides". Reviews of Geophysics 25, n.º 5 (1987): 847. http://dx.doi.org/10.1029/rg025i005p00847.

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19

Langdon, M. "Turning tides". Engineering & Technology 4, n.º 15 (12 de septiembre de 2009): 52. http://dx.doi.org/10.1049/et.2009.1508.

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20

Miller, Benjamin T., Andrew H. Lin, Susan C. Clark, Andrew P. Cap y Joseph J. Dubose. "Red tides". Journal of Trauma and Acute Care Surgery 85 (julio de 2018): S134—S139. http://dx.doi.org/10.1097/ta.0000000000001831.

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21

Maas, Leo R. M. y Arjen Doelman. "Chaotic Tides*". Journal of Physical Oceanography 32, n.º 3 (marzo de 2002): 870–90. http://dx.doi.org/10.1175/1520-0485(2002)032<0870:ct>2.0.co;2.

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22

Palumbo, A. "Atmospheric tides". Journal of Atmospheric and Solar-Terrestrial Physics 60, n.º 3 (febrero de 1998): 279–87. http://dx.doi.org/10.1016/s1364-6826(97)00078-3.

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23

Loughlin, Danielle T. "Changing Tides". Trends in Cancer 6, n.º 9 (septiembre de 2020): 717–18. http://dx.doi.org/10.1016/j.trecan.2020.07.008.

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24

JARVIS, LISA M. "CHANGING TIDES". Chemical & Engineering News 84, n.º 29 (17 de julio de 2006): 23–25. http://dx.doi.org/10.1021/cen-v084n029.p023.

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25

Mardling, Rosemary A. "Bodily Tides". EPJ Web of Conferences 11 (2011): 03002. http://dx.doi.org/10.1051/epjconf/20101103002.

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26

Mardling, Rosemary A. "Bodily Tides". EPJ Web of Conferences 11 (2011): 03002. http://dx.doi.org/10.1051/epjconf/20111103002.

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27

Zetler, B. D. y R. E. Flick. "Predicted Extreme High Tides for Mixed-Tide Regimes". Journal of Physical Oceanography 15, n.º 3 (marzo de 1985): 357–59. http://dx.doi.org/10.1175/1520-0485(1985)015<0357:pehtfm>2.0.co;2.

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28

Gou, Xiaoxiao, Huidi Liang, Tinglu Cai, Xinkai Wang, Yining Chen y Xiaoming Xia. "The Impact of Coastline and Bathymetry Changes on the Storm Tides in Zhejiang Coasts". Journal of Marine Science and Engineering 11, n.º 9 (20 de septiembre de 2023): 1832. http://dx.doi.org/10.3390/jmse11091832.

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Coastal evolutions are expected to have a significant impact on storm tides, disproportionately aggravating coastal flooding. In this study, we utilize a nested storm tide model to provide an integrated investigation of storm tide responses to changes in coastline and bathymetry along the Zhejiang coasts. We selected coastline and bathymetry data from 1980 and 2016, as well as data from three typical typhoon events (i.e., Winnie, Haikui, and Chan-hom) for simulating the storm surge processes. The results indicate that changes in the coastline and bathymetry from 1980 to 2016 have resulted in an increase in storm tides in the northern part and a decrease in the central part of Zhejiang. Specifically, storm tides in Hangzhou Bay have increased significantly, with an average increase of about 0.3 m in the maximum storm tides primarily attributed to coastline changes. On the contrary, in smaller basins like Sanmen Bay, while reclamation itself has reduced peak storm surges, rapid siltation has consequently exacerbated the storm surge. By decomposing storm tides into astronomical tides and storm surges, we discovered that the change in tidal levels was twice as significant as the surge change. Moreover, the nonlinear tide–surge interaction was nearly four times that of the pure surge, significantly contributing to storm surge variation. Alterations in the momentum balance reveal that the water depth-induced bottom friction and wind stress increase contributes to the local enlargement of storm tides at the bay head, while the coastline changes exaggerate nearshore storm tides through an increase in the advection term.

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29

Cook, Alan. "Book Review: Understanding the Tides: Tides: A Scientific History". Journal for the History of Astronomy 31, n.º 1 (febrero de 2000): 69–70. http://dx.doi.org/10.1177/002182860003100106.

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30

Yuliati, Y., E. Sumiarsih, Efawani, M. Fauzi y G. Suryo. "Water Quality and Its Relationship to Tides and Ebbs on the Sail River, Pekanbaru City, Riau Province, Indonesia". IOP Conference Series: Earth and Environmental Science 934, n.º 1 (1 de noviembre de 2021): 012072. http://dx.doi.org/10.1088/1755-1315/934/1/012072.

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Abstract The Sail River flows through the Pekanbaru City area which functions as a hydrological reservoir and main drainage channel. This river is affected by tides. Development along the Sail River Basin may affects the aquatic ecosystems. The research was conducted to determine the quality of the Sail River water and how it relates to the tides. Sampling was carried out two times during June-July 2021 in high and low tide conditions. The water quality parameters measured were temperature, TSS, pH, dissolved oxygen, BOD, COD, oil and fat, and Pb metal. Results showed that the temperature, COD, and Pb were significantly different at high tide and low tide conditions. On the other hand, during low and high tides condition, the value of TSS, pH, dissolved oxygen, BOD, oil, and fat were not significantly different. Dissolved oxygen levels during high and low tide ranged from 2.00 -3.00 mg/l and 1.00 -1.70 mg/l respectively. The Pb content during high and low tides ranged from 0.12-0.16 mg/l. In the present study, the values of dissolved oxygen and Pb content does not meet the water quality standards of Government Regulation No. 22/2021 (Class III).

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31

ROBERTSON, ROBIN. "Baroclinic and barotropic tides in the Weddell Sea". Antarctic Science 17, n.º 3 (17 de agosto de 2005): 461–74. http://dx.doi.org/10.1017/s0954102005002890.

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Barotropic and baroclinic tides were simulated for the Weddell Sea using ROMS. The model estimates for both tidal elevations and velocities showed good agreement with existing observations. The rms differences were 9 cm for elevations and 1.2–1.7 cm s−1 for the major axes of the tidal ellipses for the semidiurnal constituents and 6–8 cm and 4.5 cm s−1 for the diurnal constituents, respectively. Most of the discrepancies occurred deep under the ice shelf for the semidiurnal tides and along the continental slope for the diurnal tides. Along the continental slope, the model overestimated the generation of diurnal continental shelf waves. The diurnal tides were barotropic throughout the basin. However, internal tides were generated at semidiurnal frequencies over rough topography. Over the continental slope, semidiurnal baroclinic tidal generation was enhanced by the existence of continental shelf waves, through their harmonics. Baroclinic tides generated over rough topography in the northern Weddell Sea incited inertial oscillations as they propagated south. These inertial oscillations varied with depth since they were incited at different depths at different times as the internal tide progressed. Both the baroclinic tides and inertial oscillations induced vertical shear in the water column and increased the divergence of the horizontal surface velocities.

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32

Goring, Derek G. y Roy A. Walters. "Ocean‐tide loading and Earth tides around New Zealand". New Zealand Journal of Marine and Freshwater Research 36, n.º 2 (junio de 2002): 299–309. http://dx.doi.org/10.1080/00288330.2002.9517087.

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33

Kelly, S. M. y J. D. Nash. "Internal-tide generation and destruction by shoaling internal tides". Geophysical Research Letters 37, n.º 23 (diciembre de 2010): n/a. http://dx.doi.org/10.1029/2010gl045598.

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34

Zhao, Zhongxiang, Matthew H. Alford, James B. Girton, Luc Rainville y Harper L. Simmons. "Global Observations of Open-Ocean Mode-1 M2 Internal Tides". Journal of Physical Oceanography 46, n.º 6 (junio de 2016): 1657–84. http://dx.doi.org/10.1175/jpo-d-15-0105.1.

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AbstractA global map of open-ocean mode-1 M2 internal tides is constructed using sea surface height (SSH) measurements from multiple satellite altimeters during 1992–2012, representing a 20-yr coherent internal tide field. A two-dimensional plane wave fit method is employed to 1) suppress mesoscale contamination by extracting internal tides with both spatial and temporal coherence and 2) separately resolve multiple internal tidal waves. Global maps of amplitude, phase, energy, and flux of mode-1 M2 internal tides are presented. The M2 internal tides are mainly generated over topographic features, including continental slopes, midocean ridges, and seamounts. Internal tidal beams of 100–300 km width are observed to propagate hundreds to thousands of kilometers. Multiwave interference of some degree is widespread because of the M2 internal tide’s numerous generation sites and long-range propagation. The M2 internal tide propagates across the critical latitudes for parametric subharmonic instability (28.8°S/N) with little energy loss, consistent with the 2006 Internal Waves across the Pacific (IWAP) field measurements. In the eastern Pacific Ocean, the M2 internal tide loses significant energy in propagating across the equator; in contrast, little energy loss is observed in the equatorial zones of the Atlantic, Indian, and western Pacific Oceans. Global integration of the satellite observations yields a total energy of 36 PJ (1 PJ = 1015 J) for all the coherent mode-1 M2 internal tides. Finally, satellite observed M2 internal tides compare favorably with field mooring measurements and a global eddy-resolving numerical model.

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35

McPhee, Jack J., Peter Freewater, William Gladstone, Margaret E. Platell y Maria J. Schreider. "Glassfish switch feeding from thalassinid larvae to crab zoeae after tidal inundation of saltmarsh". Marine and Freshwater Research 66, n.º 11 (2015): 1037. http://dx.doi.org/10.1071/mf14202.

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Saltmarsh-dwelling grapsid crabs release free-swimming larvae (i.e. zoeae) into ebbing tides during spring-tide cycles that inundate saltmarshes, where initial inundation is a cue for larval release on subsequent inundations. In a saltmarsh environment, crab zoeae are the main food for fish (including the glassfish, Ambassis jacksoniensis), which ‘fast’ at other times. This saltmarsh-feeding model was tested by obtaining glassfish from near saltmarshes in a reasonably unmodified tributary of a large temperate estuary on flood and ebb tides during the night in two spring-tide events in austral autumn of 2009. Glassfish fed only on ebbing tides, with stomachs being similarly full on both spring-tide events. Thalassinid larvae (including Trypaea australiensis) dominated the dietary volumes, especially on the night before saltmarsh inundation, presumably being released during inundation of intertidal mud and sand habitats. Although glassfish progressively ‘switched’ to feeding on greater volumes of crab zoeae (presumably released after inundation of a saltmarsh) over both spring-tide cycles, such zoeal contributions never exceeded those of thalassinid larvae. The above differences highlight that, although ebb tides trigger feeding by glassfish, this ambassid focuses on different prey in a reasonably unmodified environment. The ability of glassfish to switch prey, and thus accommodate environmental differences, helps explain their high abundance in estuaries of this region.

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36

Barkho, Jouseph. "Tides of change". University of Western Ontario Medical Journal 82, n.º 2 (30 de julio de 2014): 4–5. http://dx.doi.org/10.5206/uwomj.v82i2.4557.

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The paradigm of medical resident duty hours is currently undergoing vast changes, as research has demonstrated the negative effects of sleep deprivation on the wellbeing of both patients and residents alike. These changes began in the United States, where reduced work hour schedules for residents have been implemented within the past decade. However, the effectiveness of these changes has been debated in the literature. In Canada, this issue has only recently come into spotlight. Under the guidance of the Royal College of Physicians and Surgeons of Canada, a task force was assembled in 2012 with two main objectives: gather all evidence related to resident duty hours, fatigue, and patient safety, and to create a national Canadian consensus on resident duty hours.

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37

Raloff, Janet. "Taming Toxic Tides". Science News 162, n.º 22 (30 de noviembre de 2002): 344. http://dx.doi.org/10.2307/4013946.

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38

Hagen, W. M. "The Infinite Tides". World Literature Today 86, n.º 6 (2012): 62. http://dx.doi.org/10.1353/wlt.2012.0151.

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39

Link, Denise y Lois Wessel. "Time and Tides". Journal for Nurse Practitioners 18, n.º 4 (abril de 2022): 351–52. http://dx.doi.org/10.1016/j.nurpra.2022.02.021.

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40

Mulla, Christopher M., David C. Lieb, Raymie McFarland y Joseph A. Aloi. "Tides of Change". Journal of Diabetes Science and Technology 9, n.º 3 (17 de diciembre de 2014): 602–8. http://dx.doi.org/10.1177/1932296814563953.

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41

Kushnir, Doron, Matias Zaldarriaga, Juna A. Kollmeier y Roni Waldman. "Dynamical tides reexpressed". Monthly Notices of the Royal Astronomical Society 467, n.º 2 (1 de febrero de 2017): 2146–49. http://dx.doi.org/10.1093/mnras/stx255.

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42

Sigmund, Karl y Martin A. Nowak. "Tides of tolerance". Nature 414, n.º 6862 (noviembre de 2001): 403–5. http://dx.doi.org/10.1038/35106672.

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43

Harris, A. "Taming the tides". Engineering & Technology 7, n.º 12 (1 de diciembre de 2012): 38–41. http://dx.doi.org/10.1049/et.2012.1211.

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44

Crew, E. W. "Theory of tides". Electronics and Power 33, n.º 11-12 (1987): 687. http://dx.doi.org/10.1049/ep.1987.0417.

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45

Kantha, Lakshmi H. y Craig C. Tierney. "Global baroclinic tides". Progress in Oceanography 40, n.º 1-4 (enero de 1997): 163–78. http://dx.doi.org/10.1016/s0079-6611(97)00028-1.

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46

Swinbanks, David. "Controlling the tides". Nature 348, n.º 6300 (noviembre de 1990): 381. http://dx.doi.org/10.1038/348381b0.

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47

Brink, Susanne. "Tides of change". Trends in Plant Science 6, n.º 1 (enero de 2001): 1. http://dx.doi.org/10.1016/s1360-1385(00)01830-6.

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48

Wisdom, Jack y Jennifer Meyer. "Dynamic Elastic Tides". Celestial Mechanics and Dynamical Astronomy 126, n.º 1-3 (4 de abril de 2016): 1–30. http://dx.doi.org/10.1007/s10569-016-9682-3.

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49

Logue, Marshall W. "Nucleosides/Tides Abstracts". Nucleosides and Nucleotides 4, n.º 4 (septiembre de 1985): 539–43. http://dx.doi.org/10.1080/07328318508081299.

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50

Logue, Marshall W. "Nucleosides/Tides Abstracts". Nucleosides and Nucleotides 5, n.º 4 (agosto de 1986): 457–60. http://dx.doi.org/10.1080/07328318608068686.

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