Principles of Hindu Reckoning - Revision history

en>ELApro: Martin Levey, Marvin Petruck, "Kūshyār Ibn Labbān: Principles of Hindu Reckoning" (1965)

2014-12-25T18:31:44Z

Martin Levey, Marvin Petruck, "Kūshyār Ibn Labbān: Principles of Hindu Reckoning" (1965)

← Older revision		Revision as of 20:31, 25 December 2014
Line 1:		Line 1:
			A ten foot hunk of rope can come in handy when you have to tie back a leg to keep game positioned on its back while area dressing. That is nearly a necessity with elk, simply because of the scale of the animal. The rope can also [http://www.thebestpocketknifereviews.com/best-throwing-knives-top-recommendations/ Cheap Throwing Knives] be used to tug elk quarters quick distances or for hanging gadgets from tree limbs. A knife can be important if the hunt has succeeded. Nonetheless, you don't need a big bowie knife for subject dressing. A 4 inch mounted or lock blade knife is all that's required for field dressing and even deboning an elk.<br><br>Yes, even [http://Www.Cartercountymarket.com/ccm-webid/item.php?id=27167&mode=1 Stainless Steel] knives ought to be cleaned and oiled. This is because the Stainless steel used for knives has components included in it to make it stronger and more sturdy. This makes the stainless more corrosion resistant slightly than corrosion proof. Schrade is so assured within the quality of their knives that each one comes with a Lifetime Warranty towards defects in supplies and workmanship. Moreover, the Uncle Henry knife is guaranteed for 1 full year against loss since Schrade is so assured you will prefer it so much you may be further careful not to lose it.<br><br>This stainless-steel knife liner lock folding knife was made right right here within the USA and includes a 3" false double edged blade. The handle is metal with an elongated triangle carved into either side. Unfolded, the knife measures at 7", folded it measures 4". Every knife comes with it is personal hand sewn denim drawstring pouch, dyed black right here in home. Restricted to 25 pieces. Searching for the very best survival knife to your needs can be a job that is simpler said than done. There are a ton of survival knives in the marketplace and even more opinions on what must be the thought-about the most effective survival knife<br><br>The M1903A3 Springfield rifle, otherwise known as the United States Rifle, Caliber30-06, was a service rifle issued to U.S. troops from 1905 to 1937. The 1903A3 is a bolt-motion, clip-fed rifle with an effective range of 650 yards. With such a rich American history, the rifle is commonly collected by army surplus enthusiasts. As with all weapons, periodic upkeep is crucial in order for the rifle to stay in optimum situation. This may occasionally embrace removing the barrel from the receiver. A barrel wrench - if not available - might be created from scratch with applicable machine tools.<br><br>Comply with the directions on the drywall compound container for drying occasions. After each layers of the mud have completely dried, you may now need to use a nice sanding paper to lightly clean it out. Earlier than you start this final step, though [http://www.thebestpocketknifereviews.com/best-throwing-knives-top-recommendations/ Throwing Knives For Beginners], you should put on a mask over your nostril and mouth. Once you begin sanding, the mud is admittedly going to fly, and you do not wish to breathe it into your lungs! The divot on either facet of the micarta slabs assists the consumer in bow-drill firemaking, to stabilize the top of your stick.<br><br>International - in case you can inform me the regulation relating to sending a knife and you're keen to pay value for delivery, then contact me. You may additionally be liable to import tax your end. The design standards was for a sensible anddependable customized made survival knife with a 4"(100mm) blade remaininglight and slim sufficient to be carried unobtrusively on the belt or tucked into acargo or rucksack pocket. Compact but capable. The design has been proven andtested to good effect over many seasons in a number of the world's mostinhospitable environments. RWL powdered metallurgy metal. G10 handle. Fullslotted tang. Leather-based sheath. ------------------------- Gerber Prodigy<br><br>At Sunday's listening to, though, she was alert and intent , asking for her bond to be decreased. Choose Richard Russo denied her request. MEMPHIS, Tenn. - A Memphis teen who police say studied close-fight battle ways and sharpened his knife the evening earlier than he fatally stabbed his highschool principal pleaded responsible to second-degree homicide Tuesday. Eduardo Marmolejo, 18, advised Prison Court Judge W. Mark Ward that he accepted a plea deal and a 35-yr sentence with out parole. He then apologized to the family of Suzette York, whom he stabbed a number of times and left for lifeless in a pool of blood in a classroom on Aug. 10, 2011.

	~~Never artificially weaken the counter arguments~~ in ~~order~~ to ~~make your arguments strong~~. The ~~essay will likely~~ be ~~produced~~ from ~~a certain dilemma~~, ~~and even will~~ need a ~~certain form, just like contrast~~ and ~~compare or evaluate~~. ~~In writing College Application Essay~~, ~~the students may also tell about themselves that will capture the attention of the readers~~. ~~We strive~~ to be ~~a world essay writing company through providing quality services at a price which~~ is ~~equivalent with our services. Now the writing an essay has become the big issue~~ because if the ~~person is not writing an essay of his or her own or~~ for ~~any body then this does not mean only that he or she do not know how~~ to ~~write~~ it ~~down but~~ the ~~thing~~ is that ~~there are many circumstances because of which most of~~ the ~~people cannot write~~ it ~~down~~. <br><br>~~Well there are some of~~ the ~~tips that are not mostly common~~. ~~This will make your life much easier~~, ~~and your teacher or professor will love you for not having to strain to read what you attempted to squeeze between lines~~ in ~~illegible scribble~~. ~~Custom essay writing services today can produce anything ranging from originally researched and written term papers, theses and essays~~ to ~~articles and blogs~~ for ~~people, organizations, websites and individuals based on their~~ needs ~~and requirements~~. ~~Results~~ are ~~best interpreted if the writer has~~ a ~~good grasp~~ of ~~what~~ the ~~topic is~~ and ~~is exposed enough to similar data. Custom essay writing may cause~~ the ~~sceptic in you to raise~~ the ~~alarm.~~ <br><br>~~It is like asking~~ a ~~top History student~~ to ~~complete a batch of quadratic equations~~. It is ~~good to have~~ a ~~lot of pertinent quotes in a final draft~~, ~~but keep in mind that no more than 10~~-~~15% of your written research paper should consist~~ of ~~quotations~~. ~~The company has~~ the ~~services of~~ the ~~best equipped editing team that has access~~ to ~~the best non-plagiarism software. Our essays are 100 percent genuine and we make sure each essay is unique and written~~ in ~~a different way~~. ~~will vary to~~ the ~~length of~~ the ~~essay and the amount of background information the context requires~~. <br><br>~~What makes~~ the ~~argument that 'essay writing is an art' hold water, however, is~~ the ~~fact that a considerable number~~ of ~~those who struggle with~~ the ~~writing essay task are not necessarily daft people in general terms~~, ~~but rather people who simply happen~~ to ~~lack aptitude in the fine art that is essay writing~~. ~~Such reliable companies employ professionally qualified and experienced essay writers in their respective fields of specialization~~. ~~There is~~ a ~~big difference of arguments in college essay~~ and ~~high school essay because the level of education differs a lot~~. ~~The clients feedback ensures that~~ the ~~writers conducting the academic custom essay writing have eliminated all the errors. In order~~ to ~~strongly support~~ the ~~viewpoint you hold about~~ the ~~topic~~, ~~this argument should be~~ the ~~most convincing piece~~ of ~~evidence~~. <br><br>By the ~~time [of thefrom thewith theon thein the] course [jobswork] accomplishment~~, ~~the students [usuallygenerallytypicallynormallycommonly] are supposed [~~to ~~getto obtainto haveto acquirefor getting] [requiredneedednecessary] essay writing skills, [as well asin addition toalong~~ with~~] creative [methodtechniqueapproachprocedureprocess] [in thewithin theinside~~ the~~] realm of academic writing~~. ~~Today, there are~~ many ~~companies those offering essay writing services. Narrative Essay writing: It is the simplest form~~ of ~~essay writing where~~ the ~~writer directly puts forth his personal experience & views as well~~. ~~Essay writing is one form of communication~~ and ~~it represents your point of view~~. ~~If you adored this information~~ and ~~you would like~~ to ~~receive even more details regarding [http://ace~~-~~esports~~.~~de/index~~.~~php?mod=users&action=view&id=386 buy an essay cheap] kindly go to the internet site~~. ~~Introduction part should be able~~ to ~~capture~~ the ~~attention~~ of ~~readers~~.

en>John of Reading: /* Multiplcation */Typo fixing, replaced: mulitiplication → multiplication using AWB

2014-02-27T09:54:08Z

Multiplcation: Typo fixing, replaced: mulitiplication → multiplication using AWB

← Older revision		Revision as of 11:54, 27 February 2014
Line 1:		Line 1:
	~~{{One source\|date=November 2010}}~~

	~~'''Paleosalinity''' (or Palaeosalinity) is the salinity of the global ocean or of an [[ocean basin]] at a point in geological history.~~

	~~== Importance ==~~		Never artificially weaken the counter arguments in order to make your arguments strong. The essay will likely be produced from a certain dilemma, and even will need a certain form, just like contrast and compare or evaluate. In writing College Application Essay, the students may also tell about themselves that will capture the attention of the readers. We strive to be a world essay writing company through providing quality services at a price which is equivalent with our services. Now the writing an essay has become the big issue because if the person is not writing an essay of his or her own or for any body then this does not mean only that he or she do not know how to write it down but the thing is that there are many circumstances because of which most of the people cannot write it down. <br><br>Well there are some of the tips that are not mostly common. This will make your life much easier, and your teacher or professor will love you for not having to strain to read what you attempted to squeeze between lines in illegible scribble. Custom essay writing services today can produce anything ranging from originally researched and written term papers, theses and essays to articles and blogs for people, organizations, websites and individuals based on their needs and requirements. Results are best interpreted if the writer has a good grasp of what the topic is and is exposed enough to similar data. Custom essay writing may cause the sceptic in you to raise the alarm. <br><br>It is like asking a top History student to complete a batch of quadratic equations. It is good to have a lot of pertinent quotes in a final draft, but keep in mind that no more than 10-15% of your written research paper should consist of quotations. The company has the services of the best equipped editing team that has access to the best non-plagiarism software. Our essays are 100 percent genuine and we make sure each essay is unique and written in a different way. will vary to the length of the essay and the amount of background information the context requires. <br><br>What makes the argument that 'essay writing is an art' hold water, however, is the fact that a considerable number of those who struggle with the writing essay task are not necessarily daft people in general terms, but rather people who simply happen to lack aptitude in the fine art that is essay writing. Such reliable companies employ professionally qualified and experienced essay writers in their respective fields of specialization. There is a big difference of arguments in college essay and high school essay because the level of education differs a lot. The clients feedback ensures that the writers conducting the academic custom essay writing have eliminated all the errors. In order to strongly support the viewpoint you hold about the topic, this argument should be the most convincing piece of evidence. <br><br>By the time [of thefrom thewith theon thein the] course [jobswork] accomplishment, the students [usuallygenerallytypicallynormallycommonly] are supposed [to getto obtainto haveto acquirefor getting] [requiredneedednecessary] essay writing skills, [as well asin addition toalong with] creative [methodtechniqueapproachprocedureprocess] [in thewithin theinside the] realm of academic writing. Today, there are many companies those offering essay writing services. Narrative Essay writing: It is the simplest form of essay writing where the writer directly puts forth his personal experience & views as well. Essay writing is one form of communication and it represents your point of view. If you adored this information and you would like to receive even more details regarding [http://ace-esports.de/index.php?mod=users&action=view&id=386 buy an essay cheap] kindly go to the internet site. Introduction part should be able to capture the attention of readers.
	~~From [[Bjerrum plot]]s, it is found that a decrease~~ in ~~the salinity of an aqueous fluid~~ will ~~act to increase the value of the carbon dioxide-carbonate system equilibrium constants~~, ~~(pK*). This means that the relative proportion of [[carbonate]] with respect to carbon dioxide is higher in more salinity fluids~~, e.~~g. [[seawater]]~~, ~~than in fresher waters. Of crucial importance for [[paleoclimatology]] is~~ the ~~observation~~ that ~~an increase in [[salinity]]~~ will ~~thus reduce~~ the ~~[[solubility]]~~ of ~~carbon dioxide in~~ the ~~oceans~~. ~~Since there is thought~~ to ~~have been~~ a ~~120m depression in sea level~~ at the ~~last glacial maximum due to~~ the ~~extensive formation~~ of ~~[[ice sheet]]s (which are solely freshwater),~~ this ~~represents a significant fractionation towards saltier seas during glacial periods. Correspondingly, this will cause a net outgassing of carbon dioxide into~~ the ~~atmosphere~~ because of ~~its reduced solubility, acting to increase atmospheric carbon dioxide by 6.5[[permille\|‰]]. This is thought to partly offset~~ the ~~net decrease of 80-100‰ observed during glacial periods~~.<~~ref~~>{{cite journal \| title = Glacial/interglacial variations in Carbon Dioxide \| journal = Nature \| first = D.M. \| last = Sigman \| coauthors = E.A. Boyle \| volume = 407\| id = \| url = http://www.up.ethz.ch/education/biogeochem_cycles/reading_list/sigman_nat_00.pdf \| format = PDF \| accessdate = 2010-05-17 \| pmid=11057657 \| doi=10.1038/35038000 \| year = 2000 \| issue = 6806 \| pages = 859–869}}<~~/ref~~>

	~~=== Stratification ===~~
	In addition, it is thought that extensive salinity stratification can lead to a reduction in the [[meridional overturning circulation]] (MOC) through the slowing of thermohaline circulation. Increased stratification means that there ~~is effectively a barrier to subduction~~ of ~~parcels of water; [[isopycnal]]s effectively do no outcrop at~~ the ~~surface and~~ are ~~parallel to the surface~~. ~~The ocean, in this case, can be described as "less ventilated"~~, and ~~this has been implicated in the slowing down of the MOC.~~

	~~== Measuring Paleosalinity ==~~
	~~There may exist proxies~~ for ~~salinity, but~~ to ~~date the main way that salinity has been measured has been by directly measuring [[chlorinity]]~~ in ~~[[pore fluid]]s~~.~~<ref>{{cite journal \| doi = 10.1126/science.1076252 \| title = The Salinity, Temperature~~, and ~~delta 18O of the Glacial Deep Ocean \| journal = Science \| first = J.F. \| last = Adkins \| coauthors = McIntyre, K.~~ and ~~Schrag~~, D.P. \| volume = 298 \| issue = 5599 \| pages = 1769–73 \| year = 2002 \| pmid = 12459585\| id = \| url = http://schraglab.unix.fas.harvard.edu/publications/CV49.pdf \| format = PDF \| accessdate = 2010-05-17 \| bibcode=2002Sci...298.1769A}}</ref> Adkins et al. (2002) used pore fluid chlorinity in [[Ocean Drilling Program\|ODP]] cores, ~~with the paleo-depth estimated from nearby coral horizons~~. ~~Chlorinity was measured rather than pure salinity because~~ the ~~major ions in seawater are not constant with depth in~~ the ~~sediment column; for example, sulphate reduction~~ and ~~cation-clay interactions can change overall salinity, whereas chlorinity~~ is ~~not heavily affected~~.

	~~== Paleosalinity during~~ the ~~Last Glacial Maximum ==~~
	~~Adkins' study found that global salinity increased with a global sea level drop of 120m~~. ~~Analyzing~~ <~~sup~~>18<~~/sup~~>~~O data they also found that deep waters were within error~~ of ~~the freezing point, with oceanic waters exhibiting~~ a ~~greater degree~~ of ~~homogeneity~~ in ~~temperatures. In contrast~~, ~~variations~~ in ~~salinity were much greater~~ than ~~they are today. Modern day salinities are all within 0.5 [[Practical salinity unit\|psu]]~~ of ~~the global average salinity~~ of 34.~~7 psu, whereas salinities during~~ the ~~last glacial maximum (LGM) ranged from 35.8 psu in~~ the ~~North Atlantic~~ to ~~37.1 in~~ the ~~Southern Ocean~~.

	~~There~~ are ~~some notable differences in the hydrography at the LGM~~ and ~~present day. Today the North Atlantic Deep Water ([[NADW]])~~ is ~~observed to be more saline than Antarctic Bottom Water ([[AABW]]), whereas at the last glacial maximum it was observed that the AABW was~~ in ~~fact more saline;~~ a ~~complete reversal~~. ~~Today~~ the ~~NADW is more salty because~~ of the ~~Gulf Stream; this could thus indicate a reduction~~ of ~~flow through~~ the ~~Florida Straits due to lowered sea level~~.

	~~Another observation~~ is ~~that the Southern Ocean was vastly more salty at the LGM than today~~, ~~and noticeably more salty. This~~ is ~~particularly intriguiging given~~ the ~~assumed importance~~ of the ~~[[Southern Ocean]]~~ in ~~oceanic dynamical regulation of ice ages~~. ~~The extreme value~~ of 37.~~1 psu~~ is ~~assumed to be~~ a ~~consequence~~ of ~~an increased degree of sea ice formation~~ and ~~export. This would account for~~ the ~~increased salinity, but would also account for the lack~~ of ~~oxygen isotopic fractionation; [[brine]] rejection without oxygen isotopic fractionation is thought to be highly characteristic of sea ice formation~~.

	~~===~~ The ~~increased role of salinity ===~~
	~~The presence of waters near~~ the ~~freezing point alters~~ the ~~balance of~~ the ~~relative effects of contrasts in salinity and temperature on sea water density~~. ~~This is described in~~ the ~~equation~~,
	~~:<math>\frac{\Delta\rho}{\rho}=\alpha\Delta T-\beta\Delta S</math>~~
	~~where~~ <~~math~~>~~\alpha~~<~~/math~~> is the [[~~thermal expansion coefficient~~]~~] and <math>\beta</math> is~~ the [[~~haline contraction coefficient~~]]~~. In particular~~, the ~~ratio <math>\frac{\beta}{\alpha}</math> is crucial~~. ~~Using the observed temperatures and salinities~~, ~~in the modern ocean, <math>\frac{\beta}{\alpha}</math> is about 10 whilst at the LGM <math>\frac{\beta}{\alpha}</math> it is estimated to have been closer to 25~~. ~~The modern [[thermohaline circulation]]~~ is ~~thus more controlled by density contrasts due to thermal differences, whereas during~~ the ~~LGM~~ the ~~oceans were more than twice~~ as ~~sensitive to differences in salinity rather than temperature~~. In this ~~way, the thermohaline circulation can be considered~~ to ~~have been less "thermo" and~~ more ~~"haline".~~

	~~== See also ==~~
	* [[Fresh water]]
	* [[Seawater]]
	* [[Thermohaline circulation]]

	~~== References ==~~
	~~{{reflist}}~~

	~~== External links ==~~
	*[http://~~www~~.~~salinometry~~.~~com/salinity-history History~~ of ~~salinity~~.]

	~~[[Category:Chemical oceanography]]~~
	~~[[Category:Aquatic ecology]]~~
	~~[[Category:Oceanography]]~~
	~~[[Category:Coastal geography]]~~

en>Yobot: WP:CHECKWIKI error fixes using AWB (9475)

2013-09-11T11:38:04Z

WP:CHECKWIKI error fixes using AWB (9475)

← Older revision		Revision as of 13:38, 11 September 2013
Line 1:		Line 1:
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			'''Paleosalinity''' (or Palaeosalinity) is the salinity of the global ocean or of an [[ocean basin]] at a point in geological history.

			== Importance ==
			From [[Bjerrum plot]]s, it is found that a decrease in the salinity of an aqueous fluid will act to increase the value of the carbon dioxide-carbonate system equilibrium constants, (pK*). This means that the relative proportion of [[carbonate]] with respect to carbon dioxide is higher in more salinity fluids, e.g. [[seawater]], than in fresher waters. Of crucial importance for [[paleoclimatology]] is the observation that an increase in [[salinity]] will thus reduce the [[solubility]] of carbon dioxide in the oceans. Since there is thought to have been a 120m depression in sea level at the last glacial maximum due to the extensive formation of [[ice sheet]]s (which are solely freshwater), this represents a significant fractionation towards saltier seas during glacial periods. Correspondingly, this will cause a net outgassing of carbon dioxide into the atmosphere because of its reduced solubility, acting to increase atmospheric carbon dioxide by 6.5[[permille\|‰]]. This is thought to partly offset the net decrease of 80-100‰ observed during glacial periods.<ref>{{cite journal \| title = Glacial/interglacial variations in Carbon Dioxide \| journal = Nature \| first = D.M. \| last = Sigman \| coauthors = E.A. Boyle \| volume = 407\| id = \| url = http://www.up.ethz.ch/education/biogeochem_cycles/reading_list/sigman_nat_00.pdf \| format = PDF \| accessdate = 2010-05-17 \| pmid=11057657 \| doi=10.1038/35038000 \| year = 2000 \| issue = 6806 \| pages = 859–869}}</ref>

			=== Stratification ===
			In addition, it is thought that extensive salinity stratification can lead to a reduction in the [[meridional overturning circulation]] (MOC) through the slowing of thermohaline circulation. Increased stratification means that there is effectively a barrier to subduction of parcels of water; [[isopycnal]]s effectively do no outcrop at the surface and are parallel to the surface. The ocean, in this case, can be described as "less ventilated", and this has been implicated in the slowing down of the MOC.

			== Measuring Paleosalinity ==
			There may exist proxies for salinity, but to date the main way that salinity has been measured has been by directly measuring [[chlorinity]] in [[pore fluid]]s.<ref>{{cite journal \| doi = 10.1126/science.1076252 \| title = The Salinity, Temperature, and delta 18O of the Glacial Deep Ocean \| journal = Science \| first = J.F. \| last = Adkins \| coauthors = McIntyre, K. and Schrag, D.P. \| volume = 298 \| issue = 5599 \| pages = 1769–73 \| year = 2002 \| pmid = 12459585\| id = \| url = http://schraglab.unix.fas.harvard.edu/publications/CV49.pdf \| format = PDF \| accessdate = 2010-05-17 \| bibcode=2002Sci...298.1769A}}</ref> Adkins et al. (2002) used pore fluid chlorinity in [[Ocean Drilling Program\|ODP]] cores, with the paleo-depth estimated from nearby coral horizons. Chlorinity was measured rather than pure salinity because the major ions in seawater are not constant with depth in the sediment column; for example, sulphate reduction and cation-clay interactions can change overall salinity, whereas chlorinity is not heavily affected.

			== Paleosalinity during the Last Glacial Maximum ==
			Adkins' study found that global salinity increased with a global sea level drop of 120m. Analyzing <sup>18</sup>O data they also found that deep waters were within error of the freezing point, with oceanic waters exhibiting a greater degree of homogeneity in temperatures. In contrast, variations in salinity were much greater than they are today. Modern day salinities are all within 0.5 [[Practical salinity unit\|psu]] of the global average salinity of 34.7 psu, whereas salinities during the last glacial maximum (LGM) ranged from 35.8 psu in the North Atlantic to 37.1 in the Southern Ocean.

			There are some notable differences in the hydrography at the LGM and present day. Today the North Atlantic Deep Water ([[NADW]]) is observed to be more saline than Antarctic Bottom Water ([[AABW]]), whereas at the last glacial maximum it was observed that the AABW was in fact more saline; a complete reversal. Today the NADW is more salty because of the Gulf Stream; this could thus indicate a reduction of flow through the Florida Straits due to lowered sea level.

			Another observation is that the Southern Ocean was vastly more salty at the LGM than today, and noticeably more salty. This is particularly intriguiging given the assumed importance of the [[Southern Ocean]] in oceanic dynamical regulation of ice ages. The extreme value of 37.1 psu is assumed to be a consequence of an increased degree of sea ice formation and export. This would account for the increased salinity, but would also account for the lack of oxygen isotopic fractionation; [[brine]] rejection without oxygen isotopic fractionation is thought to be highly characteristic of sea ice formation.

			=== The increased role of salinity ===
			The presence of waters near the freezing point alters the balance of the relative effects of contrasts in salinity and temperature on sea water density. This is described in the equation,
			:<math>\frac{\Delta\rho}{\rho}=\alpha\Delta T-\beta\Delta S</math>
			where <math>\alpha</math> is the [[thermal expansion coefficient]] and <math>\beta</math> is the [[haline contraction coefficient]]. In particular, the ratio <math>\frac{\beta}{\alpha}</math> is crucial. Using the observed temperatures and salinities, in the modern ocean, <math>\frac{\beta}{\alpha}</math> is about 10 whilst at the LGM <math>\frac{\beta}{\alpha}</math> it is estimated to have been closer to 25. The modern [[thermohaline circulation]] is thus more controlled by density contrasts due to thermal differences, whereas during the LGM the oceans were more than twice as sensitive to differences in salinity rather than temperature. In this way, the thermohaline circulation can be considered to have been less "thermo" and more "haline".

			== See also ==
			* [[Fresh water]]
			* [[Seawater]]
			* [[Thermohaline circulation]]

			== References ==
			{{reflist}}

			== External links ==
			*[http://www.salinometry.com/salinity-history History of salinity.]

			[[Category:Chemical oceanography]]
			[[Category:Aquatic ecology]]
			[[Category:Oceanography]]
			[[Category:Coastal geography]]

en>SchreiberBike: Link repair: Jordanus nemorarius -> Jordanus de Nemore - You can help!

2012-07-07T20:16:26Z

Link repair: Jordanus nemorarius -> Jordanus de Nemore - You can help!

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