The information presented here is placed in the public domain, and was written by Doug Burke. The notebook used to create this page is available, and questions can be asked using the GitHub issues page or via Twitter: https://twitter.com/doug_burke.
... or at least, a little bit of each.
Although I mention a few bits and pieces below, I'm going to leave it to Ned Wright's Cosmology Tutorial to explain things properly. Ned's javascript Cosmology Calculator should also be preferred to any of the code presented here, as I am ignoring some things (e.g. the contribution of neutrinos).
This is not intended to be a Haskell tutorial, rather it is meant as an example showing that it is possible to use Haskell for Astronomy. Haskell is rather different to the computer languages commonly used in Astronomy, so I try and provide Python equivalents as I go along. One thing I am not going to do is try and convince you that Haskell is the one true language for Astronomy, since it isn't. I also don't think that many of the selling points of functional programming, or using a static typing system with type inference, can easily be shown in an IHaskell notebook.
If you are interested in learning more about Haskell, then I suggest you look at one of the several guides to Haskell out there on the internet, such as Chris Allen's Learn Haskell, How to Learn Haskell, and Stephen Diehl's "What I wish I knew when learning Haskell". The newly-renovated Haskell home page is also a useful resource.
In [1]:
import Data.Time
getCurrentTime
I was recently re-reading the paper
"Experience Report: Type-checking Polymorphic Units for Astrophysics Research in Haskell"
by Takayuki Muranushi and Richard A. Eisenberg (Haskell Symposium 2014, Gothenburg, Sweden)
and wanted to try out the
units package. I have some (private) code that calculates
cosmological quantities (distance, time, volume) that uses a different approach for handling
units in Haskell (via the
dimensional
package), and thougt I'd try converting the code to use units
. Then I thought, I should
put it online for all to see - an a moment of perhaps ill-advised grandeur - and so here we are.
Unfortunately, during the development of this notebook, I found that I can't actually build
the units
module (since I am using the default ghc
version provided by Ubuntu 14.10, which
is version 7.6.3), so I ended up using a variant of the dimensional
package.
I had best point out that the following is not going to present a robust, well-thought out, API for a Cosmology library!
This is an
IHaskell
notebook, which uses the notebook features of
IPython to support an interactive Haskell environment.
Now, Haskell compilers tend to provide an interactive environment - commonly known as a
repl
- but the
advantage of IHaskell is the HTML support and easy display of non-textual items (so,
similar to why people like IPython notebooks when there's the ipython
command-line
environment).
Since this is an interactive environment, there are several differences to how code would be written and run in compiled code, but we can ignore these for now.
This section can be skipped if you are not interested in trying the code out.
For this analysis, I am using the default set of packages on my Ubuntu 14.10 machine: ghc
version 7.6.3, the
Haskell compiler, and cabal-install
(at version 1.20.0), which is used for package management (e.g. is is something like pip
).
Later versions should (hopefully) work, but earlier versions may not (the cabal sandbox
command needs a cabal-install
version of at least 1.18 and I don't know how well ghc version 7.4 or earlier are going to work).
With these installed, and having moved to a new directory, I set up a "sandbox" environment in which to install the Haskell packages (to avoid conflicting packages and to make it easy to remove or update changes for just this project), and enter
% cabal update
% cabal sandbox init
% cabal install integration chart-diagrams ihaskell ihaskell-blaze --dry-run
Resolving dependencies...
In order, the following would be installed (use -v for more details):
Boolean-0.2.3
NumInstances-1.4
...
% cabal install integration chart-diagrams ihaskell ihaskell-blaze
Resolving dependencies...
Notice: installing into a sandbox located at
/home/dburke/posts/cosmo/.cabal-sandbox
Downloading Boolean-0.2.3...
Downloading NumInstances-1.4...
Downloading OneTuple-0.2.1...
...
... and wait quite a while
...
This will create (if it doesn't already) the directory ~/.cabal/
as well as .cabal-sandbox/
in the current directory.
At this point you should be able to say
% cabal repl
GHCi, version 7.6.3: http://www.haskell.org/ghc/ :? for help
Loading package ghc-prim ... linking ... done.
Loading package integer-gmp ... linking ... done.
Loading package base ... linking ... done.
Prelude> import Numeric.Integration.TanhSinh
Prelude Numeric.Integration.TanhSinh> :quit
Leaving GHCi.
which checks that things are set up correctly.
We now need to run IHaskell, which will then set up its own version of IPython (unless it can find one it is able to use), and store it in ~/.ihaskell/
.
% mkdir notebooks
% cabal exec IHaskell -- notebook --serve=notebooks/
Did not detect IHaskell-installed or system IPython.
IHaskell will now proceed to install IPython (locally for itself).
Installing IPython in IHaskell's virtualenv in 10 seconds. Ctrl-C to cancel.
...
... this will install into ~/.ihaskell
...
Successfully installed ipython-2.4.1
Creating IPython profile.
...
... normal ipython notebook output
...
2015-02-09 19:28:24.287 [NotebookApp] The IPython Notebook is running at: http://localhost:8778/
2015-02-09 19:28:24.287 [NotebookApp] Use Control-C to stop this server and shut down all kernels (twice to skip confirmation).
At this point you should be able to go the URL where the server is running and start a notebook to follow along. If you just want to try a few things out, then the Try Haskell! and FP Complete sites provide on-line environments for trying out Haskell.
For reference, the versions of the major packages used in this notebook are (dimensional-tf
is added in later):
cabal exec ghc-pkg -- list | egrep -i 'ihaskell|integration|dimensional|chart'
Chart-1.3.3
Chart-diagrams-1.3.3
dimensional-tf-0.3.0.1
ihaskell-0.4.3.0
ihaskell-blaze-0.1.0.0
integration-0.2.0.1
Here I just load in a few modules that will be used later, for displaying
a graph. In Haskell, the form import a
loads all the symbols defined for
export from the module a
; that is, it is like Python's from a import *
.
There are ways to import just one or more symbols, or
to load in a module using a qualified name, both of which are used later.
In [2]:
import IHaskell.Display
import Graphics.Rendering.Chart.Backend.Diagrams
import Graphics.Rendering.Chart.Easy
Normally we would just install the
ihaskell-charts
package and not have to bother with this, but version 0.1.0.0
of
this package does not build with version 1.3
of
Chart. There is a fix
for this on the GitHub version of ihaskell-charts
but it's also
possible to write it directly by converting the output of Chart
into a form that the
ihaskell-blaze
package knows how to display.
In [3]:
-- For the purposes of this notebook you do not need to understand this
-- block. It may be useful to point out that in Haskell, comments are
-- introduced by "--" (or bracketed by "{-" and "-}", but I don't plan
-- to use that style here).
--
instance IHaskellDisplay (Renderable a) where
display renderable = do
(svg, _) <- renderableToSVG renderable 450 300
-- now let blaze worry about displaying the SVG
display svg
I want to calculate the angular-diameter distance to a source, so that I can find out what the projected separation between two points is when all I know is a redshift and an angle. The parameters we are interested in are the redshift of the source, $z$, the matter-density ($\Omega_m$), the vacuum-density ($\Omega_\lambda$), and Hubble's constant ($H_0$).
The angular-diameter distance, $d_A$, is
$$d_A (z; \Omega_m, \Omega_\lambda) = \frac{c}{H_0} \frac{d_c(z; \Omega_m, \Omega_\lambda)}{1+z}$$where $d_c$ is the comoving distance to the source. For simplicity, I am going to assume that we are only interested in flat cosmologies; that is, where $\Omega_m + \Omega_\lambda = 1$ (i.e. $\Omega_k = 0$), which leaves me to calculate:
$$d_A (z; \Omega_m) = \frac{c}{H_0} \frac{\int_0^z f(z; \Omega_m) dz}{1+z}$$where
$$f (z; \Omega_m) = 1 / \sqrt{ (1+z)^2 (1 + \Omega_m z) - (2+z) (1-\Omega_m) z }$$So, I start by defining the $f$ function, which has arguments of $\Omega_m$ (om
)
and redshift (z
):
In [4]:
-- Calculate f(z; omega_m). The first argument is the matter density
-- and the second the redshift.
f :: Double -> Double -> Double
f om z = let ol = 1 - om
t = (1 + z)^2 * (1 + om*z) - (2 + z) * ol * z
in 1 / sqrt t
There are several things to note here:
The first two lines are comments.
The third line gives the signature of the function: the label before ::
is the name of the
function and the types of the arguments are separated by the arrows (->
), with the last
type being the value calculated by the function. So, f
takes two Double
values and
returns a Double
.
This signature line is not required, since the Haskell compiler can determine the types.
However the types it infers a more general than the ones I gave (it has worked out that
both Float
or Double
could be used). I chose to force Double
since the integration
routine I use below works on Double
types and it simplifies some of the discussion
below, such as when asking for the type of the g
function.
The function arguments on line four are separated by spaces rather than brackets and commas.
The definition of the function (lines four to siz) uses the let xxx in yyy
form, which defines a set of
local symbols (in this case ol
and t
) which are then used to calculate a value.
Function application does not use brackets, so the denominator of the fraction is
just sqrt t
. However, precedence rules means that brackets may be needed to clarify
what is an argument. For instance, if I had not used the temporary symbol t
then I would
have had to write 1 / sqrt ((1 + z)^2 * (1 + om*z) - (2 + z) * ol * z)
.
The above is similar to the Python code:
def f(om,z):
ol = 1 - om
t = (1 + z)**2 * (1 + om*z) - (2 + z) * ol * z
return 1 / math.sqrt(t)
I now want to check how $f$ varies with redshift for a given $\Omega_m$ value (in this case
I want to use a value of 0.3
, since that is close to the
currently-preferred cosmological
model). I can do this by
taking advantage of
partial application to easily create a function
that calls f
with the first argument fixed to 0.3
:
In [5]:
g = f 0.3
The Python version would be something like
def g(z):
return f(0.3, z)
or
g = lambda z: f(0.3, z)
Since I am often going to be interested in how things vary with redshift, I am going to
make this parameter the last one, so that it makes it easy to partially apply
the functions I write (as in the case of making g
a specialized version of f
).
The :type
command - which is part of the interactive Haskell environment rather than
Haskell itself - reports the type of a symbol: in this case it shows us that g
is
a function that takes a Double
and returns a Double
(so it has one less "Double ->
"
term than f
).
In [6]:
:type g
:type f
I am going to gloss over the fact that Haskell functions only ever accept a single argument, using curried functions to implement what appear to be multi-argument functions. It is an important point to understand if you are going to be writing Haskell, but I don't want to derail the discussion too much.
Getting back to the code, I can evaluate g
for $z=0$ and then $z=1.2$
(taking advantage of the automatic-display capabilities of the
IHaskell notebook; in an actual Haskell program we would have to say something like print (g 0)
to display the value):
In [7]:
g 0
In [8]:
g 1.2
I want to evaluate this function for a number of different redshifts, so I want to
automate this process, which leads to lists and the map
function.
In Haskell, lists of objects are represented by comma-separated values enclosed by
[]
brackets - e.g. [1.2, 3.4, 9.8]
- and have a type of [a]
, where a
is the
type of the list element. The map
function takes a function which accepts one
argument, as well as a list of arguments, and returns a list of values created
by applying the function to each argument. That is, it has a type of:
In [9]:
:type map
For this discussion we can ignore the forall a b
part of the type.
To be general, the function supplied to map can have different types for its input and output lists,
(so a
and b
above)
but here we will use g
which means that the input and output lists have a type
of [Double]
:
In [10]:
:type map g
which means that the following evaluates g
with z=0
, z=0.4
, and z=3.2
:
In [11]:
map g [0, 0.4, 3.2]
I want to look at g
evaluated for a range of redshits
between 0 and 10, so let's create the list of redshifts
(a common scheme when naming
variables in Haskell is to add a s
for a list of values, hence the
use of zs
here) and evaluate g
on each element:
In [12]:
zs = [0::Double, 0.1 .. 10]
gs = map g zs
The form [a, a+dx .. b]
is similar to NumPy's numpy.arange(a, b+dx, dx)
, so this is similar to the Python/NumPy code
zs = numpy.arange(0, 10.1, 0.1)
# You could use Python's map
gs = map(g, zs)
# or a list compreshension
gs = [g(z) for z in zs]
Note that I am ignoring the difference between Python lists and NumPy arrays here.
I did not need to add ::Double
to 0
when creating zs
, but did so just to keep the types "concrete". If I had said
zs = [0, 0.1 .. 10]
then gs
would still be a list of Double
values, but the type of zs
would be
forall t. (Enum t, Fractional t) => [t]
and I don't really want to try and explain
Haskell type classes
(the names to the left of the =>
) here.
We can finally take advantage of the display code I wrote at the start of the notebook, and
use the routines from the
Graphics.Rendering.Chart.Easy
module
of the
Chart package
to display gs
versus zs
:
In [13]:
toRenderable (do
layout_title .= "f"
layout_x_axis . laxis_title .= "Redshift"
layout_y_axis . laxis_title .= "f(z)"
plot (line "O_matter=0.3 O_lambda=0.7" [zip zs gs])
)
This command doesn't look like anything I've shown so far, and I don't really want to explain it too much, but the
toRenderable
function takes a list of actions, which describes the plot, and converts it a value with a
Renderable
type, defined in the
Chart package,
which is itself then converted into SVG and automatically
displayed by the notebook, due to the code I wrote way back at the start.
The list of actions is created using
do
notation,
which is a way of representing a chain of actions - in this case things
like "set the X-axis label to 'Redshift'" and "plot up this list of (x,y) points" - in Haskell. This is very terse
and it's best if you just let your eyes skip over the code and focus on the plot instead.
To calculate the angular-diameter distance I need to integrate f
. The
"Why functional programming matters" (link to PDF)
article by John Hughes provides a nice implementation that highlights
some of the ways that
lazy evaluation can be used to
simplify code. However, it's easier to use a pre-canned solution,
and in this case I have chosen to use the
integration
package:
In [14]:
import Numeric.Integration.TanhSinh
There are several ways to integrate up a function, and the results can be bounded to a relative
or absolute limit. The function g
is "well behaved", so a simple integration scheme is likely
to be sufficient. The runs below - where I have approximated $\int_0^2 g(z) dz$,
show that both Simpson's and the trapezoidal methods agree,
so I shall use trap
(the absolute limit of 1.0e-6
is excessive but the run times are not
prohibitive here):
In [15]:
absolute 1.0e-6 (simpson g 0 2)
In [16]:
absolute 1.0e-6 (trap g 0 2)
The result of absolute
is a Haskell record, but all we need worry about now is that the
value of the integrated function can be retrieved from it by using result
, as shown below:
In [17]:
result (absolute 1.0e-6 (trap g 0 2))
If you are wondering what just happened: the simpson
and trap
routines take a function of one parameter (the function
to integrate, so g
here) and a range over which to integrate ($z=0$ to $z=2$ here), and return a list of approximations (the [Result]
return type) which (hopefully) converge on the answer. The absolute
routine takes a limit value and a list of results, returning the first one whose error estimate is smaller than the given limit.
In [18]:
:type simpson
:type trap
:type absolute
:type relative
We can look at these return values, using the take 3
function that returns the first three elements of a list,
to see that the result has converged quickly:
In [19]:
take 3 (trap g 0 2)
In [20]:
take 3 (simpson g 0 2)
Getting back to the task at hand, I can define daH
as a function that accepts $\Omega_m$ and $z$
and returns the angular-diameter distance, in units of the Hubble length, by saying:
In [21]:
daH om z = let fs = result (absolute 1.0e-6 (trap (f om) 0 z))
in fs / (1+z)
The equivalent Python would be something like
def daH(om,z):
# I am assuming here that the integrate and trap methods are
# defined somewhere else.
fs = integrate(lambda z: f(om,z), 0, z, method=trap, abstol=1.0e-6)
return fs / (1+z)
Although not given explicitly, the compiler can infer that the two input arguments, and the result,
have a type of Double
:
In [22]:
:type daH
As I want to plot up the angular-diameter distance as a function of redshift for several
different cosmologies, I define a helper function that, given an $\Omega_m$ value, returns
a list of $(z, dA(z))$ points, which is in the form needed by the line
command used
earlier.
In [23]:
-- This uses the list of redshifts defined earlier.
--
-- (daH om) has type Double -> Double
-- zs has type [Double]
-- so map (daH om) zs has type [Double]
--
-- zip's signature is [a] -> [b] -> [(a,b)]
-- that is, it pairs up corresponding elements of
-- the two input arrays. This means that
-- the output of zip zs (map (daH om) zs)
-- is [(Double, Double)], where the first element
-- of eachpair is the redshift, and the second element
-- the anular-diameter distance for this redshift
-- (in units of the Hubble length).
--
calcDAH om = zip zs (map (daH om) zs)
The Python equivalent would be:
def calcDAH(om):
zs = np.arange(0, 10.1, 0.1)
return [(z, daH(om,z)) for z in zs]
This can then be used to display the results for several cosmologies:
In [24]:
toRenderable (do
layout_title .= "Angular-diameter distance"
layout_x_axis . laxis_title .= "Redshift"
layout_y_axis . laxis_title .= "dA(z)"
plot (line "O_m=0.1 O_l=0.9" [calcDAH 0.1])
plot (line "O_m=0.3 O_l=0.7" [calcDAH 0.3])
plot (line "O_m=0.9 O_l=0.1" [calcDAH 0.9])
)
The plot shows the non-monotonic nature of the angular-diameter distance.
To get a value with physical units, we multiply daH
by c/
$H_0$, which,
if the speed of light is in km/s
and $H_0$ in km/s/Mpc
, will give a value
in Megaparsecs:
In [25]:
-- Calculate the angular-diameter distance for a flat Cosmology
-- with a matter density of om, Hubble constant of H0 (in km/s/Mpc),
-- and redshift. The result is in Mpc.
--
da om h0 z = daH om z * c / h0
where
-- speed of light in km/s
c = 299792.458
For variety I chose to use the form xxx where yyy
rather than let yyy in xxx
, as used in earlier examples.
This routine can then be used to calculate angular-diameter distances for a range of redshifts:
In [26]:
map (da 0.3 70) [0, 0.5, 1.0, 1.2, 2.0]
As a sanity check, I used Ned Wright's
CosmoCalc calculator and recorded
the distances for several redshifts. These are stored in the nedWrightDA
list,
and then I calculate the ratio of the distance I calculate to those from CosmoCalc
(the rel
list). As can be seen, the values are all close to 1.0.
In [27]:
nedWrightDA = [1259.0, 1651.8, 1710.5, 1726.3]
-- zipWith has a type of (a -> b -> c) -> [a] -> [b] -> [c], and
-- applies the function (first argument) to the elements in the two input
-- lists, creating the output list. Here I supply a list of redshifts
-- and a list of the values from CosmoCalc for those redshifts, and
-- then return the angular-diameter distance calculated for the
-- redshift divided by the CosmoCalc value.
--
-- The (\lambda z nw -> da 0.3 70 z / nw) fragment is Haskell syntax
-- for creating an anonymous function that takes two arguments (z and nw
-- here) and then applying the function body (in this case divide the
-- value of "da 0.3 70 z" by nw).
--
-- I could have written this in several lines, and avoided the need for
-- all these comments!
rel = zipWith (\z nw -> da 0.3 70 z / nw) [0.5, 1.0, 1.2, 2.0] nedWrightDA
rel
The Python equivalent for calculating rel
would be something like (where I have
decided to use shorter variable names than above):
da = [da(0.3,70,z) for z in [0.5, 1, 1.2, 2]]
nw = [1259.0, 1651.8, 1710.5, 1726.3]
rel = np.asarray(da) / np.asarray(nw)
I can now repeat the previous plot, this time with physical units:
In [28]:
calcDA om = zip zs (map (da om 70) zs)
toRenderable (do
layout_title .= "Angular-diameter distance; H_0 = 70 km/s/Mpc"
layout_x_axis . laxis_title .= "Redshift"
layout_y_axis . laxis_title .= "dA(z) [Mpc]"
plot (line "O_m=0.1 O_l=0.9" [calcDA 0.1])
plot (line "O_m=0.3 O_l=0.7" [calcDA 0.3])
plot (line "O_m=0.9 O_l=0.1" [calcDA 0.9])
)
To get the linear distance between two points at the same redshift, separated by an angle of theta, we can use the small-angle approximation: convert the angle to radians and then multiply it by the angular-diameter distance. Astronomers use all kinds of funny units for angles; in this case I am assuming the input angle has units of arcminutes. As there are 60 arcminutes to a degree, the conversion to radians is just $\pi / (180*60)$.
In [29]:
-- Given Omega_m, H_0 in km/s/Mpc, z, and an angle in arcminutes,
-- return the linear scale in kpc.
adist om h0 z angle = 1000 * d * a
where
-- convert angle, in arcminutes, into radians
a = pi * angle / (180 * 60)
-- d is in Mpc
d = da om h0 z
For a redshift of 2, with a closed cosmology and $\Omega_m = 0.3$, the
CosmoCalc
calculator calculate a scale of 8.370 kiloparsecs per arcsec. How close
do I get (given that one arcsec is 1/60 of an arcminute and I intentionally made
adist
return values in kpc):
In [30]:
adist 0.3 70 2 (1/60)
So, not bad agreement. As a reminder, the code I had to write to get this (stripping out all the non-essential bits, including niceties like type signatures and comments, from above) was:
f om z = let ol = 1 - om
in 1 / sqrt( (1+z)^2 * (1 + om*z) - (2+z) * ol * z )
daH om z = let fs = result (absolute 1.0e-6 (trap (f om) 0 z))
in fs / (1+z)
da om h0 z = daH om z * c / h0
where
c = 299792.458
adist om h0 z angle = 1000 * d * a
where
a = pi * angle / (180 * 60)
d = da om h0 z
If I wanted to make this code usable I would spend some time thinking about whether it is worth defining types
especially for the matter density, Hubble's constant, or redshift values, to clarify routines like adist
which take four Double
values and it is easy to mix them up - e.g. swapping om
and h0
- leading to incorrect results. However,
that's a discussion for another day.
The above calculation is fine, but I'd like to explicitly include the units in the calculation, so that you know the answer is in Mpc (or some other unit). There are several Haskell packages that support this; I have previously used the dimensional package and there is also unittyped and quantities, but today I want to try the units package. As I have not tried out the support for quantities and units in astropy I do not provide Python equivalents for the rest of this notebook.
Unfortunately, using ghc version 7.6.3 means that only the first version (1.0.0
) of units
can
be used, which is a problem, since it doesn't build! So I decided to try out the
dimensional-tf
package, since it a different approach to the dimensional
package, which I have
used. The difference between the two is not really relevant here; we can just look at
is as being one way to model quantities and units in a physical calculation in Haskell.
I hope to have time to repeat this with a more-recent version of ghc
so that I can
try out units
.
To install the necessary package we need to use cabal
again:
cabal install dimensional-tf --dry-run
... check that no problems are reported
cabal install dimensional-tf
... this should be relatively quick as there's not that many
... dependencies that need to be built
The following statement is similar to Python's import foo.bar.baz as bob
statement; symbols defined by the module must be preceeded by the quaifier
P
. The reason for doing this is that this module provides versions of
common mathematical operations - such as multiplication - which would
conflict with the default versions. It will make it clear what version
I am using, but is visually distracting, as you will soon see!
In [31]:
import qualified Numeric.Units.Dimensional.TF.Prelude as P
I start by defining the speed of light, c
, in meters per second (you can use P.meter
or P.metre
here):
In [32]:
c = 299792458.0 P.*~ (P.meter P./ P.second)
The inferred type for this is confusing:
In [33]:
:type c
This can be fixed by giving an explicit type, as shown below (it's not actually necessary to do so, but I do so because I can):
In [34]:
c :: P.Velocity Double
c = 299792458.0 P.*~ (P.meter P./ P.second)
In [35]:
:type c
The type is now more readable, but in reality this is just a synonym for the original type (except that the
Fractional
constraint has been replaced by the use of an explicit type Double
, which is a member of the
Fractional
type class).
Although not relevant here - as I'm treating the module as something of a black box - the
dimensions of the value are encoded here using
Peano numbers, where Z
indicates 0
, S a
is one more than a
(so
S Z
is 1
and S (S (S Z))
is 3
),
and N a
is used to negate a
. The Dim
statement from the original type of c
can therefore
be read as Dim 1 0 -1 0 0 0 0
, so this suggests that the first element refers to length and the third refers
to time. I believe the reason for using Peano numbers here is because they are inductively defined (the base
case is 0 and the inductive step is add one), which means that the type checker can match up things as needed.
One thing to note, if you've read this far into the paragraph, is that this information is only relevant when
the code is compiled. This means that you only "pay" for the checking when you build
the code (which can, unfortunately, take some time for particularly complex cases) rather than when you run it.
More information on the API of the dimensional-tf
package
can be found in the
source code
to this module, as it uses a literate programming style which means that the comments do not
get displayed in the standard
module documentation.
The main thing to note just now is that there are types for quantities - such as the speed of light
in meters per second - and for units - such as second. These types are labelled
Quantity
or Unit
and contain the relevant dimension information (the Dim
type seen above)
and the type of the numerical value (e.g. Double
). Synonyms are used to make these
more readable, such as Velocity
meaning Quantity DVelocity
and
DVelocity
being Dim (S Z) Z (N (S Z)) Z Z Z Z
, which can sometimes be a bit confusing
when you are trying to work out how everything fits together.
The symbol c
now retains both the quantity and the units, as displaying it shows:
In [36]:
c
The quantity stored in c
can be extracted, converting to a given unit, using the /~
operator,
as shown below (note that this is one point where the use of the P
prefix is visually distracting):
In [37]:
c P./~ (P.kilo P.meter P./ P.second)
Using it in a calculation is also somewhat unsatisfting, since you need to use the mathematical
operators from the module - leading to visual clutter if you use the approach I have taken
here - and the need to use constants such as P._2
to represent the value 2
:
In [38]:
c P./ P._2
Alternatively, I can "convert" a value into a dimensionless number by using the form value *~ one
(which is needed
when there is no pre-defined constant):
In [39]:
c P./ (2 P.*~ P.one)
Here I define a symbol that represents one arcminute. The use of 1::Double
is just to make sure that this is a Double
value, rather than a more general one, in a similar manner to how c
was defined.
In [40]:
arcmin = (1::Double) P.*~ P.minuteOfArc
In [41]:
:type arcmin
One of the reasons for using a system which also encodes units is to make it an error for combining incompatible values; in this case trying to add together the speed of light and an angle is an error. Admittedly, a rather confusing one if you're not used to the Haskell type system.
In [42]:
arcmin + c
I guess that the "native" value for angles is radians, so let's check this:
In [43]:
arcmin
which is one arcminute in radians, since:
In [44]:
pi / (60 * 180)
I can also check that the numerical values are equal directly, by
using /~ radian
to extract then numeric value from arcmin
:
In [45]:
arcmin P./~ P.radian == (pi / (60*180))
If I had not "converted" arcmin
from a quantity to a standard value, using /~ radian
, then
I would have come across another rather frightening error message:
In [46]:
arcmin == (pi / (60*180))
I want to be able to handle lengths which contain parsecs, so I need to create a unit
for this, using the prefix
function:
In [47]:
parsec :: P.Unit P.DLength Double
parsec = P.prefix 3.085678e16 P.metre
With this, I can now create distances in units of mega parsecs:
In [48]:
3.2 P.*~ P.mega parsec
and even define a unit for the Hubble constant:
In [49]:
hubbleConstant :: P.Unit P.DFrequency Double
hubbleConstant = P.kilo P.meter P./ P.second P./ P.mega parsec
I included the explicit type to make things a bit more readable - the
inferred value is
Dimensional DUnit (Dim Z Z (N (S Z)) Z Z Z Z) Double
- and also to ensure that the equation I used is sensible (i.e. that
the units are correct). As an example, if I had missed out the "per second"
part then I would have got the following error (I promise that you can,
with enough experience, work out what's going on from these error messages):
In [50]:
wrongConstant :: P.Unit P.DFrequency Double
wrongConstant = P.kilo P.meter P./ P.mega parsec
When the hubbleConstant
is applied to a value, the result has a type of Quantity DFrequency Double
,
as shown below:
In [51]:
70 P.*~ hubbleConstant
In [52]:
:type 70 P.*~ hubbleConstant
Since I will want to use this type a few times below, I define an alias for it, using the type
command. After this, I can use HConstant
to simplify signatures of functions that take
a Hubble constant as a parameter; I also add in a Length
alias, since this will also
come in useful.
In [53]:
type HConstant = P.Quantity P.DFrequency Double
type Length = P.Quantity P.DLength Double
With these definitions I should now be able to replicate the angular-diameter calculation, but this time tracking the types as well. As a reminder, I want:
f om z = let ol = 1 - om
in 1 / sqrt( (1+z)^2 * (1 + om*z) - (2+z) * ol * z )
daH om z = let fs = result (absolute 1.0e-6 (trap (f om) 0 z))
in fs / (1+z)
da om h0 z = daH om z * c / h0
where
c = 299792.458
adist om h0 z angle = 1000 * d * a
where
a = pi * angle / (180 * 60)
d = da om h0 z
Since f
and daH
are dimensionless, I'll just re-use them and concentrate on
da
and adist
.
There are four main points in the conversion of da
:
I added a signature to ensure that the Hubble constant has the required units. This trades off generic behavior (accepting any quantity) against some measure of type safety (in the sense that I want to make sure the second argument has the units of Hubble's constant). The results below would not change if I did not give the signature.
I have not had to convert c
from m/s
to km/s
(or, equivalently,
explictly convert the Hubble constant to account for the use of both
km
and Mpc
).
The value returned by daH
is converted to a dimensionless quantity
by "multiplying" it by one
.
The result does not look too different from the original form.
In [54]:
da2 :: Double -> HConstant -> Double -> Length
da2 om h0 z = (daH om z P.*~ P.one) P.* c P./ h0
The conversion for adist
is also simple.
In [55]:
adist2 om h0 z angle = da2 om h0 z P.* angle
Since I did not give a type signature, the inferred version does not
require that the angle be dimensionless (shown by the fact that d'
,
which represents the dimensions of the value,
is listed as forall
rather than being an explicit value):
In [56]:
:type adist2
I can fix this by explicitly specifying that the fourth argument is an angle by saying
In [57]:
adist3 :: Double -> HConstant -> Double -> P.Quantity P.DPlaneAngle Double -> Length
adist3 = adist2
The difference in type signatures can be seen if I give a non-angle value for the
last argument: the adist2
form returns a value whereas the adist3
version raises an error:
In [58]:
adist2 0.3 (70 P.*~ hubbleConstant) 2 (1 P.*~ P.meter)
In [59]:
adist3 0.3 (70 P.*~ hubbleConstant) 2 (1 P.*~ P.meter)
With this, I can repeat the earlier calculation, which gave
adist 0.3 70 2 (1/60) = 8.370893333112804
In [60]:
adist3 0.3 (70 P.*~ hubbleConstant) 2 (1 P.*~ P.secondOfArc)
Oops: I want the answer in kpc
:
In [61]:
adist3 0.3 (70 P.*~ hubbleConstant) 2 (1 P.*~ P.secondOfArc) P./~ P.kilo parsec
It is easy to change units, such as to use an angle in arcminutes and to convert
the answer to Mpc
:
In [62]:
adist3 0.3 (70 P.*~ hubbleConstant) 2 (2.4 P.*~ P.minuteOfArc) P./~ P.mega parsec
The luminosity of a source is equal to $4 \pi d_l^2 f_x$, where $d_l$ is the distance to the source and $f_x$ its flux (this assumes a bolometric flux, since it ignores the K correction).
For a source at a cosmological distance, the distance used is the luminosity distance - which is why I used the subscript $l$ - and it is defined as
$$d_l = (1+z) d_c$$
In [63]:
dlH om z = let fs = result (absolute 1.0e-6 (trap (f om) 0 z))
in fs * (1+z)
dl :: Double -> HConstant -> Double -> Length
dl om h0 z = (dlH om z P.*~ P.one) P.* c P./ h0
Trying it out, I get (using the same Cosmology as previously) a luminosity distance to an object at $z=2$ of:
In [64]:
dl 0.3 (70 P.*~ hubbleConstant) 2
which, in Astronomer friendly units, is:
In [65]:
dl 0.3 (70 P.*~ hubbleConstant) 2 P./~ P.mega parsec
The CosmoCalc page returns 15537.0 Mpc or 50.675 Gly. Now, can I easily convert the answer above to light years?
For this, I need to import the year
value from the "non SI" module of dimensional-tf
In [66]:
import Numeric.Units.Dimensional.TF.NonSI (year)
and use it - together with the definition of c
above, to calculate the distance
light travels in a year. I am not happy with the following, as I calculate a value
in meters, remove the meters, then make it into a unit of meters, but I couldn't
see how else to convert a Quantity
- which is what c * year
is - into
a Unit
.
In [67]:
lightYear = let d = c P.* (1 P.*~ year) P./~ P.meter
in P.prefix d P.meter
With this, I can convert the distance into light years to compare to the cosmoCalc
value:
In [68]:
dl 0.3 (70 P.*~ hubbleConstant) 2 P./~ P.giga lightYear
Finally it's time to create a function that converts a flux to a luminosity:
In [69]:
luminosity :: Double -> HConstant -> Double -> P.Irradiance Double -> P.RadiantIntensity Double
luminosity om h0 z flux = P._4 P.* P.pi P.* d P.* d P.* flux
where
d = dl om h0 z
As an X-ray astronomer I'm used to working in units of ergs
(please don't ask why),
so I create a few units built on this: one for flux and one for luminosity.
In [70]:
erg = P.prefix (1.0e-7::Double) P.joule
ergLum = erg P./ P.second
ergFlux = ergLum P./ P.square (P.centi P.meter)
With these I can finally calculate the luminosity of a source ($z=2$, $\Omega_m=0.3$, $\Omega_\lambda=0.7$, $H_0 = 70\ {\rm km/s/Mpc}$) which has a flux of $2 \times 10^{-13}\ {\rm erg/cm^{2}/s}$.
In [71]:
lum = luminosity 0.3 (70 P.*~ hubbleConstant) 2 (2e-13 P.*~ ergFlux)
This value is
In [72]:
lum
which can be converted to several units; such as ${\rm Watts}$
In [73]:
lum P./~ P.watt
which is - unsurprisingly - the same numerical value, or $\rm{erg / cm^2 / s}$, which has a numerical value $10^7$ times this:
In [74]:
lum P./~ ergLum
Don't forget that this would need some form of K-correction, unless you have a bolometric flux measurement.
Whilst I have your attention, how about calculating the critical density of the Universe, which is defined as:
$$\rho_{\rm crit} = \frac{3 H^2}{8 \pi G}$$For this, I need a value for the
Gravitational constant,
where the meter ^ pos3
and second ^ pos2
terms represent $m^3$ and $s^2$
respectively.
In [75]:
bigG = 6.67428e-11 P.*~ (P.metre P.^ P.pos3 P./ P.kilo P.gram P./ P.second P.^ P.pos2)
With this, I can write out the equation to calculate the critical density:
In [76]:
criticalDensity h = P._3 P.* h P.^ P.pos2 P./ (P._8 P.* P.pi P.* bigG)
Applying this to $H_0 = 70\ {\rm km/s/Mpc}$ gives:
In [77]:
c70 = criticalDensity (70 P.*~ hubbleConstant)
c70
which I can convert to other units, such as metric tons per cubed Astronomical Unit:
In [78]:
c70 P./~ (P.kilo P.metricTon P./ P.astronomicalUnit P.^ P.pos3)
The use of the P.
prefix is definitely distracting here. The way I've used the dimensional
package in the past is to have most of the code in a module, and in that module
I have imported the module directly. This means that the code can be written in
the more-natural form
criticalDensity h = _3 * h ^ pos2 / (_8 * pi * bigG)
The downside to this is that normal arithmetic becomes more verbose.
There you go; I hope you enjoyed it. If you have any questions, then please use the GitHub issues page or contact me on Twitter at https://twitter.com/doug_burke.