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The '''geostrophic wind''' ({{IPAc-en|icon|dʒ|iː|ɵ|ˈ|s|t|r|ɒ|f|ɨ|k}} or {{IPAc-en|dʒ|iː|ɵ|ˈ|s|t|r|oʊ|f|ɨ|k}}) is the [[theoretical]] [[wind]] that would result from an exact balance between the [[Coriolis effect]] and the [[pressure gradient]] force.  This condition is called ''geostrophic balance.'' The geostrophic wind is directed [[Parallel (geometry)|parallel]] to [[isobar (meteorology)|isobar]]s (lines of constant [[Atmospheric pressure|pressure]] at a given height). This balance seldom holds exactly in nature.  The true wind almost always differs from the geostrophic wind due to other forces  such as [[friction]] from the ground. Thus, the actual wind would equal the geostrophic wind only if there were no friction and the isobars were perfectly straight. Despite this, much of the atmosphere outside the [[tropics]] is close to geostrophic flow much of the time and it is a valuable first approximation. Geostrophic flow in air or water is a zero-frequency [[inertial waves|inertial wave]].
In mathematics, the '''Iwahori–Hecke algebra''', or '''Hecke algebra''',  named for [[Erich Hecke]] and [[Nagayoshi Iwahori]], is a one-parameter deformation of the [[group algebra]] of a [[Coxeter group]].


==Origin==
Hecke algebras are quotients of the group rings of [[Artin braid group]]s. This connection found a spectacular application in [[Vaughan Jones]]' construction of [[Jones polynomial|new invariants of knots]]. Representations of Hecke algebras led to discovery of [[quantum group]]s by [[Michio Jimbo]]. [[Michael Freedman]] proposed Hecke algebras as a foundation for [[topological quantum computer|topological quantum computation]].


[[Air]] naturally moves from areas of high [[pressure]] to areas of low pressure, due to the [[pressure gradient]] force.  As soon as the air starts to move, however, the [[Coriolis effect|Coriolis "force"]] deflects it.  The {{wict|deflection}} is to the right in the [[northern hemisphere]], and to the left in the [[southern hemisphere]].  As the air moves from the high pressure area, its speed increases, and so does its Coriolis deflection.  The deflection increases until the Coriolis and pressure gradient forces are in geostrophic balance: at this point, the air flow is no longer moving from high to low pressure, but instead moves along an {{wict|isobar}}. (Note that this explanation assumes that the atmosphere starts in a geostrophically unbalanced state and describes how such a state would evolve into a balanced flow. In practice, the flow is nearly always balanced.) The geostrophic balance helps to explain why, in the northern hemisphere, [[low pressure system]]s (or ''[[cyclone]]s'') spin counterclockwise and [[High pressure area|high pressure systems]] (or ''[[anticyclone]]s'') spin clockwise, and the opposite in the southern hemisphere.
==Hecke algebras of Coxeter groups==
Start with the following data:


==Geostrophic currents==
* ''(W,S)'' is a [[Coxeter system]] with the Coxeter matrix ''M = (m<sub>st</sub>)'',
* ''R'' is a commutative ring with identity.
* {''q<sub>s</sub>'' | ''s'' &isin; ''S''} is a family of units of ''R'' such that ''q<sub>s</sub>'' = ''q<sub>t</sub>'' whenever ''s'' and ''t'' are conjugate in ''W''
* ''A'' is the ring of [[Laurent polynomial]]s over '''Z''' with indeterminates ''q<sub>s</sub>'' (and the above restriction that ''q<sub>s</sub>'' = ''q<sub>t</sub>'' whenever ''s'' and ''t'' are conjugated), that is ''A'' = '''Z''' [''q''{{su|p=±1|b=s}}]


Flow of ocean water is also largely geostrophic. Just as multiple weather balloons that measure pressure as a function of height in the atmosphere are used to map the atmospheric pressure field and infer the geostrophic wind, measurements of density as a function of depth in the ocean are used to infer geostrophic currents. [[satellite altimetry|Satellite altimeters]] are also used to measure sea surface height anomaly, which permits a calculation of the geostrophic current at the surface.
===Multiparameter Hecke Algebras===
The ''multiparameter Hecke algebra'' ''H<sub>R</sub>(W,S,q)'' is a unital, associative ''R''-algebra with generators ''T<sub>s</sub>'' for all ''s'' &isin; ''S'' and relations:
* '''Braid Relations:''' ''T<sub>s</sub> T<sub>t</sub> T<sub>s</sub>'' ... = ''T<sub>t</sub> T<sub>s</sub> T<sub>t</sub>'' ..., where each side has ''m<sub>st</sub>'' < &infin; factors and ''s,t'' belong to ''S''.
* '''Quadratic Relation:''' For all ''s'' in ''S'' we have: (''T<sub>s</sub>'' - ''q<sub>s</sub>'')(''T<sub>s</sub>'' + 1) = 0.


==Limitations of the Geostrophic approximation==
'''Warning''': in recent books and papers, Lusztig has been using a modified form of the quadratic relation that reads <math>(T_s-q_s^{1/2})(T_s+q_s^{-1/2})=0.</math> After extending the scalars to include the half integer powers ''q''{{su|p=±½|b=s}} the resulting Hecke algebra is isomorphic to the previously defined one (but the ''T<sub>s</sub>'' here corresponds to ''q''{{su|p=½|b=s}} ''T''<sub>s</sub> in our notation). While this does not change the general theory, many formulae look different.


The effect of friction, between the air and the land, breaks the geostrophic balance. Friction slows the flow, lessening the effect of the Coriolis force. As a result, the pressure gradient force has a greater effect and the air still moves from high pressure to low pressure, though with great deflection. This explains why high pressure system winds radiate out from the center of the system, while low pressure systems have winds that spiral inwards.
===Generic Multiparameter Hecke Algebras===
''H<sub>A</sub>(W,S,q)'' is the ''generic'' multiparameter Hecke algebra. This algebra is universal in the sense that every other multiparameter Hecke algebra can be obtained from it via the (unique) ring homomorphism ''A'' → ''R'' which maps the indeterminate ''q<sub>s</sub>'' &isin; ''A'' to the unit ''q<sub>s</sub>'' &isin; ''R''. This homomorphism turns ''R'' into a ''A''-algebra and the scalar extension ''H<sub>A</sub>(W,S)'' &otimes;<sub>''A''</sub> ''R'' is canonically isomorphic to the Hecke algebra ''H<sub>R</sub>(W,S,q)'' as constructed above. One calls this process ''specialization'' of the generic algebra.


The geostrophic wind neglects [[friction]]al effects, which is usually a good [[approximation]] for the [[synoptic scale meteorology|synoptic scale]] instantaneous flow in the midlatitude mid-[[troposphere]].<ref>Holton, J.R., 'An Introduction to Dynamic Meteorology', International Geophysical Series, Vol 48 Academic Press.</ref> Although [[ageostrophic]] terms are relatively small, they are essential for the time evolution of the flow and in particular are necessary for the growth and decay of storms. Quasigeostrophic and Semigeostrophic theory are used to model flows in the atmosphere more widely. These theories allow for divergence to take place and for weather systems to then develop.
=== One-parameter Hecke Algebras ===
If one specializes every indeterminant ''q<sub>s</sub>'' to a single indeterminant ''q'' over the integers (or ''q''{{su|p=½|b=s}} to ''q''<sup>½</sup> respectively), then one obtains the so-called generic one-parameter Hecke algebra of ''(W,S)''.


==Governing formula==
Since in Coxeter groups with single laced Dynkin diagrams (for example groups of type A and D) every pair of Coxeter generators is conjugated, the above mentioned restriction of ''q<sub>s</sub>'' being equal ''q<sub>t</sub>'' whenever ''s'' and ''t'' are conjugated in ''W'' forces the multiparameter and the one-parameter Hecke algebras to be equal. Therefore it is also very common to only look at one-parameter Hecke algebras.
Newton's Second law can be written as follows if only the pressure gradient, gravity, and friction act on an air parcel, where the bold symbolizes a vector.


<math>{D\boldsymbol{U} \over Dt} = -2\boldsymbol{\Omega} \times \boldsymbol{U} - {1 \over \rho} \nabla p + \boldsymbol{g} + \boldsymbol{F}_r</math>
=== Coxeter groups with weights ===
If an integral weight function is defined on ''W'' (i.e. a map ''L:W'' → '''Z''' with ''L(vw)=L(v)+L(w)'' for all ''v,w'' &isin; ''W'' with ''l(vw)=l(v)+l(w)''), then a common specialization to look at is the one induced by the homomorphism ''q<sub>s</sub>'' ↦ ''q<sup>L(s)</sup>'', where ''q'' is a single indeterminant over '''Z'''.


Where F<sub>r</sub> is the friction and ''g'' is the [[standard gravity|acceleration due to gravity]] (9.81 m.s<sup>−2</sup>).
If one uses the convention with half-integer powers, then weight function ''L:W'' → ½'''Z''' may be permitted as well. For technical reasons it is also often convenient only to consider positive weight functions.


Locally this can be expanded in cartesian coordinates, with a positive u representing an eastward direction and a positive v representing a northward direction. Neglecting friction and vertical motion, we have:
== Properties ==
1. The Hecke algebra has a basis <math>(T_w)_{w\in W}</math> over ''A'' indexed by the elements of the Coxeter group ''W''. In particular, ''H'' is a free ''A''-module. If <math>w=s_1 s_2 \ldots s_n</math> is a [[reduced decomposition]] of ''w'' &isin; ''W'', then <math>T_w=T_{s_1}T_{s_2}\ldots T_{s_n}</math>. This basis of Hecke algebra is sometimes called the '''natural basis'''. The [[neutral element]] of ''W'' corresponds to the identity of ''H'': ''T<sub>e</sub>'' = 1.


<math>{Du \over Dt} = -{1 \over \rho}{\partial P \over \partial x} + f \cdot v</math>
2. The elements of the natural basis are ''multiplicative'', namely, ''T''<sub>yw</sub>=''T''<sub>y</sub> ''T''<sub>w</sub> whenever ''l(yw)=l(y)+l(w)'', where ''l'' denotes the [[length function]] on the Coxeter group ''W''.


<math>{Dv \over Dt} = -{1 \over \rho}{\partial P \over \partial y} - f \cdot u</math>
3. Elements of the natural basis are invertible. For example, from the quadratic relation we conclude that ''T''{{su|p=-1|b=s}} = ''q''{{su|p=-1|b=s}} ''T<sub>s</sub>'' + (''q''{{su|p=-1|b=s}}-1).


<math> 0 = -g -{1 \over \rho}{\partial P \over \partial z}</math>
4. Suppose that ''W'' is a finite group and the ground ring is the field '''C''' of complex numbers. [[Jacques Tits]] has proved that if the indeterminate ''q'' is specialized to any complex number outside of an explicitly given list (consisting of roots of unity), then the resulting one parameter Hecke algebra is [[semisimple algebra|semisimple]] and isomorphic to the complex group algebra '''C'''[''W''] (which also corresponds to the specialization ''q'' ↦ 1.


With <math>f = 2 \Omega \sin{\phi}</math> the [[Coriolis effect|Coriolis parameter]] (approximately 10<sup>&minus;4</sup> s<sup>&minus;1</sup>, varying with latitude).
5. More generally, if ''W'' is a finite group and the ground ring ''R'' is a field of [[characteristic zero]], then the one parameter Hecke algebra is a [[semisimple algebra|semisimple associative algebra]] over ''R''[''q''<sup>±1</sup>]. Moreover, extending earlier results of Benson and Curtis, George Lusztig provided an explicit isomorphism between the Hecke algebra and the group algebra after the extension of scalars to the quotient field of ''R''[''q''<sup>±½</sup>]
<!--
that if ''A'' is extended to the field <math>K=R(q^{\frac12}) then the ''K''-algebra <math>H_K=H\otimes_A K</math> obtained from ''H'' by the change of scalars is isomorphic over ''K'' to the group algebra ''K[W]'' of the Coxeter group ''W''.


Assuming geostrophic balance, the system is stationary and the first two equations become:
Lusztig, George. On a theorem of Benson and Curtis. J. Algebra 71 (1981), no. 2, 490–498.
However, it seems excessive to give this reference in an article in an encyclopedia!
-->


<math>f \cdot v = {1 \over \rho}{\partial P \over \partial x}</math>
== Canonical basis ==
{{main|Kazhdan–Lusztig polynomial}}
A great discovery of Kazhdan and Lusztig was that a Hecke algebra admits a ''different'' basis, which in a way controls representation theory of a variety of related objects.


<math>f \cdot u = -{1 \over \rho}{\partial P \over \partial y}</math>
The generic multiparameter Hecke algebra, ''H<sub>A</sub>(W,S,q)'', has an involution ''bar'' that maps ''q''<sup>½</sup> to ''q''<sup>-½</sup> and acts as identity on '''Z'''. Then ''H'' admits a unique ring automorphism ''i'' that is [[semilinear transformation|semilinear]] with respect to the bar involution of ''A'' and maps ''T<sub>s</sub>'' to ''T{{su|p=-1|b=s}}''. It can further be proved that this automorphism is involutive (has order two) and takes any ''T<sub>w</sub>'' to <math>T^{-1}_{w^{-1}}.</math>


By substituting using the third equation above, we have:
<blockquote> '''Kazhdan - Lusztig Theorem:''' For each ''w'' ∈ ''W'' there exists a unique element <math>C^{\prime}_w</math> which is invariant under the involution ''i'' and if one writes its expansion in terms of the natural basis:
::<math> C'_w= \left (q^{-1/2} \right )^{l(w)}\sum_{y\leq w}P_{y,w}T_y, </math>
one has the following:
* ''P''<sub>w,w</sub>=1,
* ''P''<sub>y,w</sub> in '''Z'''[''q''] has degree less than or equal to ½''(l(w)-l(y)-1)'' if ''y<w'' in the [[Bruhat order]],
* ''P''<sub>y,w</sub>=0 if <math>y\nleq w.</math></blockquote>


<math>f \cdot v = g\frac{\partial P / \partial x}{\partial P / \partial z} = g{\partial Z \over \partial x}</math>
The elements <math>C^{\prime}_w</math> where ''w'' varies over ''W'' form a basis of the algebra ''H'', which is called the ''dual canonical basis'' of the Hecke algebra ''H''. The ''canonical basis'' {''C''<sub>w</sub> | ''w'' &isin; ''W''} is obtained in a similar way. The polynomials ''P''<sub>y,w</sub>(''q'') making appearance in this theorem are the [[Kazhdan–Lusztig polynomials]].


<math>f \cdot u = -g\frac{\partial P / \partial y}{\partial P / \partial z} = -g{\partial Z \over \partial y}</math>
The Kazhdan–Lusztig notions of left, right and two-sided ''cells'' in Coxeter groups are defined through the behavior of the canonical basis under the action of ''H''.


with ''Z'' the height of the constant pressure surface (satisfying <math>{\partial P \over \partial x}dx + {\partial P \over \partial y}dy + {\partial P \over \partial z} dZ = 0 </math>).
== Hecke algebra of a locally compact group ==
Iwahori–Hecke algebras first appeared as an important special case of a very general construction in group theory. Let ''(G,K)'' be a pair consisting of a [[unimodular group|unimodular]] [[locally compact topological group]] ''G'' and a closed subgroup ''K'' of ''G''. Then the space of ''K''-biinvariant [[continuous function]]s of [[compact support]], ''C<sub>c</sub>(K\G/K)'', can be endowed with a structure of an associative algebra under the operation of [[convolution]]. This algebra is denoted by ''H(G//K)'' and called the '''Hecke ring''' of the pair ''(G,K)''.


This leads us to the following result for the geostrophic wind components <math>(u_g,v_g)</math>:
'''Example:''' If ''G'' = SL(''n'','''Q'''<sub>''p''</sub>) and ''K'' = SL(''n'','''Z'''<sub>''p''</sub>) then the Hecke ring is commutative and its representations were studied by [[Ian G. Macdonald]]. More generally if ''(G,K)'' is a [[Gelfand pair]] then the resulting algebra turns out to be commutative.


: <math> u_g = - {g \over f}  {\partial Z \over \partial y}</math>
'''Example:''' If ''G'' = SL(2,'''Q''') and ''K'' = SL(2,'''Z''') we get the abstract ring behind [[Hecke operators]] in the theory of [[modular forms]], which gave the name to Hecke algebras in general.


<!-- extra blank line between two lines of "displayed" [[TeX]], for legiblity -->
The case leading to the Hecke algebra of a finite Weyl group is when ''G'' is the finite [[Chevalley group]] over a [[finite field]] with ''p''<sup>k</sup> elements, and ''B'' is its [[Borel subgroup]]. Iwahori showed that the Hecke ring ''H(G//B)'' is obtained from the generic Hecke algebra ''H''<sub>q</sub> of the [[Weyl group]] ''W'' of ''G'' by specializing the indeterminate ''q'' of the latter algebra to ''p''<sup>k</sup>, the cardinality of the finite field. George Lusztig remarked in 1984 (''Characters of reductive groups over a finite field'', xi, footnote):


: <math> v_g = {g \over f}  {\partial Z \over \partial x}</math>
:''I think it would be most appropriate to call it the Iwahori algebra, but the name Hecke ring (or algebra) given by Iwahori himself has been in use for almost 20 years and it is probably too late to change it now.''


The validity of this approximation depends on the local [[Rossby number]]. It is invalid at the equator, because ''f'' is equal to zero there, and therefore generally not used in the [[tropics]].
Iwahori and Matsumoto (1965) considered the case when ''G'' is a group of points of a [[reductive algebraic group]] over a non-archimedean [[local field]] ''K'', such as '''Q'''<sub>''p''</sub>, and ''K'' is what is now called an [[Iwahori subgroup]] of ''G''. The resulting Hecke ring is isomorphic to the Hecke algebra of the [[affine Weyl group]] of ''G'', or the [[affine Hecke algebra]], where the indeterminate ''q'' has been specialized to the cardinality of the [[residue field]] of ''K''.


Other variants of the equation are possible; for example, the geostrophic wind vector can be expressed in terms of the gradient of the [[geopotential height]] Φ on a surface of constant pressure:
Work of Roger Howe in the 1970s and his papers with Allen Moy on representations of ''p''-adic GL(''n'') opened a possibility of classifying irreducible admissible representations of reductive groups over local fields in terms of appropriately constructed Hecke algebras. (Important contributions were also made by Joseph Bernstein and [[Andrey Zelevinsky]].) These ideas were taken much further in [[Colin Bushnell]] and [[Philip Kutzko]]'s ''[[theory of types (mathematics)|theory of types]]'', allowing them to complete the classification in the general linear case. Many of the techniques can be extended to other reductive groups, which remains an area of active research. It has been conjectured that all Hecke algebras that are ever needed are mild generalizations of affine Hecke algebras.


: <math> \overrightarrow{V_g} = {\hat{k} \over f} \times \nabla_p \Phi </math>
== Representations of Hecke algebras ==
It follows from Iwahori's work that complex representations of Hecke algebras of finite type are intimately related with the structure of the spherical [[principal series representation]]s of finite Chevalley groups.


== See also ==
George Lusztig pushed this connection much further and was able to describe most of the characters of finite groups of Lie type in terms of representation theory of Hecke algebras. This work used a mixture of geometric techniques and various reductions, led to introduction of various objects generalizing Hecke algebras and detailed understanding of their representations (for ''q'' not a root of unity). [[Modular representation]]s of Hecke algebras and representations at roots of unity turned out to be related with the theory of canonical bases in [[affine quantum group]]s and very interesting combinatorics.
*[[Geostrophic current]]
*[[Thermal wind]]
*[[Gradient wind]]
*[[Prevailing winds]]


==References==
Representation theory of affine Hecke algebras was developed by Lusztig with a view towards applying it to description of representations of ''p''-adic groups. It is in many ways quite different in flavor from the finite case. A generalization of affine Hecke algebras, called ''double affine Hecke algebra'', was used by [[Ivan Cherednik]] in his proof of the [[Macdonald conjectures]].
{{Reflist}}


== External links ==
== References ==
* [http://atmos.nmsu.edu/education_and_outreach/encyclopedia/geostrophic.htm  Geostrophic approximation]
*David Goldschmidt [http://www.ams.org/online_bks/ulect4/ Group Characters, Symmetric Functions, and the Hecke Algebra] {{MR|1225799}},ISBN 0-8218-3220-4
* [http://nsidc.org/arcticmet/glossary/geostrophic_winds.html Definition of geostrophic wind]
*Iwahori, Nagayoshi; Matsumoto, Hideya [http://www.numdam.org/item?id=PMIHES_1965__25__5_0 ''On some Bruhat decomposition and the structure of the Hecke rings of p-adic Chevalley groups.''] Publications Mathématiques de l'IHÉS, 25 (1965), pp.&nbsp;5–48. {{MR|0185016}}
*[http://atmo.tamu.edu/class/atmo203/tut/windpres/wind8.html Geostrophic wind description]
* Alexander Kleshchev, ''Linear and projective representations of symmetric groups'', Cambridge tracts in mathematics, vol. 163. Cambridge University Press, 2005. {{MR|2165457}}, ISBN 0-521-83703-0
* George Lusztig, [http://www.ams.org/bookstore-getitem/item=CRMM-18 Hecke algebras with unequal parameters], CRM monograph series, vol.18, American Mathematical Society, 2003. {{MR|1658581}}, ISBN 0-8218-3356-1
* Andrew Mathas, [http://www.ams.org/bookstore-getitem/item=ULECT-15 Iwahori-Hecke algebras and Schur algebras of the symmetric group], University Lecture Series, vol.15, American Mathematical Society, 1999. {{MR|1711316}}, ISBN 0-8218-1926-7
* Lusztig, George, ''On a theorem of Benson and Curtis'', J. Algebra 71 (1981), no. 2, 490–498. {{MR|0630610}}, {{DOI|10.1016/0021-8693(81)90188-5}}
* Colin Bushnell and Philip Kutzko, ''The admissible dual of GL(n) via compact open subgroups'', Annals of Mathematics Studies, vol. 129, Princeton University Press, 1993. {{MR|1204652}}, ISBN 0-691-02114-7


{{DEFAULTSORT:Geostrophic Wind}}
{{DEFAULTSORT:Iwahori-Hecke algebra}}
[[Category:Geophysics]]
[[Category:Algebras]]
[[Category:Fluid dynamics]]
[[Category:Representation theory]]
[[Category:Atmospheric dynamics]]
 
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Revision as of 06:38, 12 August 2014

In mathematics, the Iwahori–Hecke algebra, or Hecke algebra, named for Erich Hecke and Nagayoshi Iwahori, is a one-parameter deformation of the group algebra of a Coxeter group.

Hecke algebras are quotients of the group rings of Artin braid groups. This connection found a spectacular application in Vaughan Jones' construction of new invariants of knots. Representations of Hecke algebras led to discovery of quantum groups by Michio Jimbo. Michael Freedman proposed Hecke algebras as a foundation for topological quantum computation.

Hecke algebras of Coxeter groups

Start with the following data:

  • (W,S) is a Coxeter system with the Coxeter matrix M = (mst),
  • R is a commutative ring with identity.
  • {qs | sS} is a family of units of R such that qs = qt whenever s and t are conjugate in W
  • A is the ring of Laurent polynomials over Z with indeterminates qs (and the above restriction that qs = qt whenever s and t are conjugated), that is A = Z [qTemplate:Su]

Multiparameter Hecke Algebras

The multiparameter Hecke algebra HR(W,S,q) is a unital, associative R-algebra with generators Ts for all sS and relations:

  • Braid Relations: Ts Tt Ts ... = Tt Ts Tt ..., where each side has mst < ∞ factors and s,t belong to S.
  • Quadratic Relation: For all s in S we have: (Ts - qs)(Ts + 1) = 0.

Warning: in recent books and papers, Lusztig has been using a modified form of the quadratic relation that reads After extending the scalars to include the half integer powers qTemplate:Su the resulting Hecke algebra is isomorphic to the previously defined one (but the Ts here corresponds to qTemplate:Su Ts in our notation). While this does not change the general theory, many formulae look different.

Generic Multiparameter Hecke Algebras

HA(W,S,q) is the generic multiparameter Hecke algebra. This algebra is universal in the sense that every other multiparameter Hecke algebra can be obtained from it via the (unique) ring homomorphism AR which maps the indeterminate qsA to the unit qsR. This homomorphism turns R into a A-algebra and the scalar extension HA(W,S)A R is canonically isomorphic to the Hecke algebra HR(W,S,q) as constructed above. One calls this process specialization of the generic algebra.

One-parameter Hecke Algebras

If one specializes every indeterminant qs to a single indeterminant q over the integers (or qTemplate:Su to q½ respectively), then one obtains the so-called generic one-parameter Hecke algebra of (W,S).

Since in Coxeter groups with single laced Dynkin diagrams (for example groups of type A and D) every pair of Coxeter generators is conjugated, the above mentioned restriction of qs being equal qt whenever s and t are conjugated in W forces the multiparameter and the one-parameter Hecke algebras to be equal. Therefore it is also very common to only look at one-parameter Hecke algebras.

Coxeter groups with weights

If an integral weight function is defined on W (i.e. a map L:WZ with L(vw)=L(v)+L(w) for all v,wW with l(vw)=l(v)+l(w)), then a common specialization to look at is the one induced by the homomorphism qsqL(s), where q is a single indeterminant over Z.

If one uses the convention with half-integer powers, then weight function L:W → ½Z may be permitted as well. For technical reasons it is also often convenient only to consider positive weight functions.

Properties

1. The Hecke algebra has a basis over A indexed by the elements of the Coxeter group W. In particular, H is a free A-module. If is a reduced decomposition of wW, then . This basis of Hecke algebra is sometimes called the natural basis. The neutral element of W corresponds to the identity of H: Te = 1.

2. The elements of the natural basis are multiplicative, namely, Tyw=Ty Tw whenever l(yw)=l(y)+l(w), where l denotes the length function on the Coxeter group W.

3. Elements of the natural basis are invertible. For example, from the quadratic relation we conclude that TTemplate:Su = qTemplate:Su Ts + (qTemplate:Su-1).

4. Suppose that W is a finite group and the ground ring is the field C of complex numbers. Jacques Tits has proved that if the indeterminate q is specialized to any complex number outside of an explicitly given list (consisting of roots of unity), then the resulting one parameter Hecke algebra is semisimple and isomorphic to the complex group algebra C[W] (which also corresponds to the specialization q ↦ 1.

5. More generally, if W is a finite group and the ground ring R is a field of characteristic zero, then the one parameter Hecke algebra is a semisimple associative algebra over R[q±1]. Moreover, extending earlier results of Benson and Curtis, George Lusztig provided an explicit isomorphism between the Hecke algebra and the group algebra after the extension of scalars to the quotient field of R[q±½]

Canonical basis

Mining Engineer (Excluding Oil ) Truman from Alma, loves to spend time knotting, largest property developers in singapore developers in singapore and stamp collecting. Recently had a family visit to Urnes Stave Church. A great discovery of Kazhdan and Lusztig was that a Hecke algebra admits a different basis, which in a way controls representation theory of a variety of related objects.

The generic multiparameter Hecke algebra, HA(W,S,q), has an involution bar that maps q½ to q and acts as identity on Z. Then H admits a unique ring automorphism i that is semilinear with respect to the bar involution of A and maps Ts to TTemplate:Su. It can further be proved that this automorphism is involutive (has order two) and takes any Tw to

Kazhdan - Lusztig Theorem: For each wW there exists a unique element which is invariant under the involution i and if one writes its expansion in terms of the natural basis:

one has the following:

The elements where w varies over W form a basis of the algebra H, which is called the dual canonical basis of the Hecke algebra H. The canonical basis {Cw | wW} is obtained in a similar way. The polynomials Py,w(q) making appearance in this theorem are the Kazhdan–Lusztig polynomials.

The Kazhdan–Lusztig notions of left, right and two-sided cells in Coxeter groups are defined through the behavior of the canonical basis under the action of H.

Hecke algebra of a locally compact group

Iwahori–Hecke algebras first appeared as an important special case of a very general construction in group theory. Let (G,K) be a pair consisting of a unimodular locally compact topological group G and a closed subgroup K of G. Then the space of K-biinvariant continuous functions of compact support, Cc(K\G/K), can be endowed with a structure of an associative algebra under the operation of convolution. This algebra is denoted by H(G//K) and called the Hecke ring of the pair (G,K).

Example: If G = SL(n,Qp) and K = SL(n,Zp) then the Hecke ring is commutative and its representations were studied by Ian G. Macdonald. More generally if (G,K) is a Gelfand pair then the resulting algebra turns out to be commutative.

Example: If G = SL(2,Q) and K = SL(2,Z) we get the abstract ring behind Hecke operators in the theory of modular forms, which gave the name to Hecke algebras in general.

The case leading to the Hecke algebra of a finite Weyl group is when G is the finite Chevalley group over a finite field with pk elements, and B is its Borel subgroup. Iwahori showed that the Hecke ring H(G//B) is obtained from the generic Hecke algebra Hq of the Weyl group W of G by specializing the indeterminate q of the latter algebra to pk, the cardinality of the finite field. George Lusztig remarked in 1984 (Characters of reductive groups over a finite field, xi, footnote):

I think it would be most appropriate to call it the Iwahori algebra, but the name Hecke ring (or algebra) given by Iwahori himself has been in use for almost 20 years and it is probably too late to change it now.

Iwahori and Matsumoto (1965) considered the case when G is a group of points of a reductive algebraic group over a non-archimedean local field K, such as Qp, and K is what is now called an Iwahori subgroup of G. The resulting Hecke ring is isomorphic to the Hecke algebra of the affine Weyl group of G, or the affine Hecke algebra, where the indeterminate q has been specialized to the cardinality of the residue field of K.

Work of Roger Howe in the 1970s and his papers with Allen Moy on representations of p-adic GL(n) opened a possibility of classifying irreducible admissible representations of reductive groups over local fields in terms of appropriately constructed Hecke algebras. (Important contributions were also made by Joseph Bernstein and Andrey Zelevinsky.) These ideas were taken much further in Colin Bushnell and Philip Kutzko's theory of types, allowing them to complete the classification in the general linear case. Many of the techniques can be extended to other reductive groups, which remains an area of active research. It has been conjectured that all Hecke algebras that are ever needed are mild generalizations of affine Hecke algebras.

Representations of Hecke algebras

It follows from Iwahori's work that complex representations of Hecke algebras of finite type are intimately related with the structure of the spherical principal series representations of finite Chevalley groups.

George Lusztig pushed this connection much further and was able to describe most of the characters of finite groups of Lie type in terms of representation theory of Hecke algebras. This work used a mixture of geometric techniques and various reductions, led to introduction of various objects generalizing Hecke algebras and detailed understanding of their representations (for q not a root of unity). Modular representations of Hecke algebras and representations at roots of unity turned out to be related with the theory of canonical bases in affine quantum groups and very interesting combinatorics.

Representation theory of affine Hecke algebras was developed by Lusztig with a view towards applying it to description of representations of p-adic groups. It is in many ways quite different in flavor from the finite case. A generalization of affine Hecke algebras, called double affine Hecke algebra, was used by Ivan Cherednik in his proof of the Macdonald conjectures.

References