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The '''moist static energy''' is a [[thermodynamic]] variable that describes the state of an [[air parcel]], and is similar to the [[equivalent potential temperature]].<ref>{{cite web |url=http://amsglossary.allenpress.com/glossary/search?id=moist-static-energy1 |author=American Meteorological Society |work=AMS Glossary |title=Moist static energy |year=2000 |accessdate=25 June 2010 }}</ref> The moist static energy is a combination of a parcels [[internal energy]] due to an air parcel's temperature, its [[potential energy]] due to its height above the surface, and the [[latent energy]] due to water vapor present in the air parcel. It is a useful variable for researching the atmosphere because, like several other similar variables, it is approximately conserved during [[Adiabatic process|adiabatic]] ascent and descent.<ref>{{cite web |url=http://www.meted.ucar.edu/tropical/textbook/ch6/moistprecip_6_2_3.html |title=Adiabatic Processes and Vertical Distribution of Moisture |work=Introduction to Tropical Meteorology |year=2010 |accessdate=25 June 2010 |author=University Corporation for Atmospheric Research }} [Requires free registration] </ref>
We usually take care of our customers custom essay help in order to give the best and outstanding essay writing help which satisfy our customers. Our services writing company provides students with different categories of essay writing. It also helped solve a huge problem with last year's application by streamlining the mechanics of applying for colleges electing to do away with separate, and sometimes overlooked, writing supplements. Referenced material, either reworded or echoed ought to be incorporated into the paper. Creating, when it comes to GCSE English (the actual exam undertaken by 16 year olds within their final 12 months in Secondary School in the U. <br><br>The company offers all kinds of medical essay writing in all subjects of medical course for the student in all academic levels. This is looked down upon as one of the major causes of getting bad grades. The introduction must be very clear and simply state what you are going to write about. Every good essay begins with a thought or argument called 'a thesis. They should be followed and tweaked so that you are producing the quality content your readers deserve. <br><br>If one wants to write an essay, but one does not know how to write one, one can take essay writing help from an expert. We ensure that our writers use diverse resource to gather information for the papers. As these writing service employ professional editors, students. Now, you have to revise your paper and find out mistakes. If you're ready to find more info in regards to [http://hotel631.server4you.net/index.php?mod=users&action=view&id=152476 do my essay cheap] look at the webpage. All those who know how to write an essay can write a good essay by keeping in mind some of the important points. <br><br>You can post them the question as it was posted to you by your professor then they know what to do. People may feel that writing an essay might be extremely difficult and complicated but it is not so. However, essay writing helps improve the students understanding on a particular topic. To help counselors keep track of which colleges and universities require the ACT with Writing and to foreshadow future decisions for colleges opting to require Writing with the new SAT, Cigus Vanni has once again authored a list based on information provided by the ACT and updated with individual website research. An essay is a short piece of writing which deals with a given topic analytically from the Authors point of view. <br><br>Write a quick schedule to help you allocate your time wisely: list the days you have left and the time during the day you will be able to work. Persuasive essay also called as argumentative essays are written for the sole purpose of convincing the readers about a particular point of view. As a result, they have to source for help in essay writing. "Knowing the truth" behind your recently rejected work will not help. A student gives their assignment to the essay writing service, and they write it for them.
 
The moist static energy, S, can be described mathematically as:
::<math>S=C_p \cdot T + g \cdot z + L_v \cdot q</math>
where C<sub>p</sub> is the [[specific heat]] at constant pressure, T is the [[Thermodynamic temperature|absolute air temperature]], g is the [[Earth's gravity|gravitational constant]], z is the height above the surface, L<sub>v</sub> is the latent heat of vaporization, and q is water vapor [[specific humidity]].<ref>{{cite book | last = Wallace | first = John | authorlink = | coauthors = Peter Hobbs | title = Atmospheric Science: An Introductory Survey (2nd ed.) | publisher = Elsevier | year = 2006 | location =  | pages = | | doi = | id = | isbn = 0-12-732951-X }}</ref><ref>{{cite journal |title=The Moist Static Energy Budget of a Composite Tropical Intraseasonal Oscillation in a Climate Model |first1=Eric D. |last1=Maloney |journal=Journal of Climate |year=2009 |volume=22 |number=3 |pages=711–729 |doi=10.1175/2008JCLI2542.1 |bibcode = 2009JCli...22..711M }}</ref> Note that many texts use mixing ratio r in place of specific humidity q because these values tend to be close (within a few percent) under normal atmospheric conditions, but this is an approximation and not strictly correct.  
 
Through the study of moist static energy profiles, [[Herbert Riehl]] and [[Joanne Malkus]] determined in 1958 that [[hot tower]]s, small cores of [[convection]] approximately {{convert|5|km|mi}} wide that extend from the [[planetary boundary layer]] to the [[tropopause]], were the primary mechanism that transported energy out of the tropics to the middle latitudes.<ref>{{cite journal |journal=Geophysica |last1=Riehl |first1=Herbert |last2=Malkus |first2=Joanne |volume=6 |number=3–4 |year=1958 |title=On the heat balance in the equatorial trough zone }}</ref> More recently, idealized model simulations of the tropics indicate that the moist static energy budget is dominated by [[advection]], with shallow inflow in the lowest {{convert|2|km|ft}} of the atmosphere with outflow concentrated about {{convert|10|km|ft}} above the surface.<ref>{{cite conference |url=http://ams.confex.com/ams/88Annual/techprogram/paper_136910.htm |title=Calculating the moist static energy budget around the ITCZ in idealized WRF simulations |first1=S.W. |last1=Powell |first2=D.S. |last2=Nolan |conference=Seventh Annual AMS Student Conference }}</ref> Moist static energy has also been used to study the [[Madden–Julian oscillation]] (MJO). As with the tropics as a whole, the budget of moist static energy in the MJO is dominated by advection, but also is influenced by the wind-driven component of the surface latent heat flux. The relationship between the advection component and the latent heat component influence the timing of the MJO.<ref>{{cite journal |title=The Moist Static Energy Budget of a Composite Tropical Intraseasonal Oscillation in a Climate Model |first1=Eric D. |last1=Maloney |journal=Journal of Climate |year=2009 |volume=22 |number=3 |pages=711–729 |doi=10.1175/2008JCLI2542.1 |bibcode = 2009JCli...22..711M }}</ref>
 
==See also==
*[[Hot tower]]
*[[Latent heat]]
*[[Western Hemisphere Warm Pool]]
 
==References==
{{Reflist}}
 
[[Category:Atmospheric thermodynamics]]

Latest revision as of 23:58, 14 April 2014

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