Chaitanya's Random Pages

January 31, 2013

Some noteworthy time zones

Filed under: geography — ckrao @ 11:10 am

I was recently learning about time zones and thought I would collect some notes about some of the more interesting ones here. In total there are 40 time zones spanning the globe.

  • UTC – 12:00: Nobody lives here (it covers the uninhabited US islands of Baker Island and Howland Island in the Pacific)
  • UTC -11:00: Samoa used to be in this time zone but it switched to UTC+13, skipping 30 December 2011 in the process.
  • UTC -9:30: Only covered by the Marquesas Islands (French Polynesia), population ~9,000.
  • UTC -4:30: Used in Venezuela since December 9 2007 (previously used UTC -4:00)
  • UTC -3:30: Used in southeastern Labrador and Newfoundland, Canada
  • UTC -1:00: Used in Cape Verde, eastern Greenland (in winter) and the Azores (Portugal, in winter)
  • UTC +3:30: Used by Iran in winter
  • UTC +4:30: Used by Afghanistan and Iran (in summer)
  • UTC +5:30: Used in India and Sri Lanka, the world’s second most populated time zone
  • UTC +5:45: Used in Nepal since 1986
  • UTC +6:30: Used in Myanmar and Cocos Islands (Australia)
  • UTC +8:45: Unofficial time zone used in Eucla and surrounds, Western Australia, population ~200
  • UTC +9:30: Used in Northern Territory, South Australia (winter), western New South Wales around Broken Hill (winter) (all in Australia)
  • UTC +10:30: Used in Lord Howe Island, South Australia (summer), western New South Wales around Broken Hill (summer) (all in Australia)
  • UTC +11:30: Used in Norfolk Island (Australia)
  • UTC +12:45: Used in Chatham Islands (New Zealand)
  • UTC +14:00: The highest time zone (used by the Line Islands of Kiribati)

Here are the time zones used in the past but not at present.

  • UTC -10:30: Used by Hawaii from 1900 to 1947 (now UTC -10:00)
  • UTC -8:30: Used in Pitcairn Islands (UK) until 1998 (now UTC -8:00)
  • UTC -0:44: Used in Liberia from 1919 to 1972 (now UTC 0:00)
  • UTC -0:25: Used in Ireland from 1880 to 1916 (now UTC 0:00 in winter)
  • UTC +0:20: Used in Netherlands from 1909 to 1940 (now UTC +1:00 in winter)
  • UTC +0:30: Sandringham time used in the British royal household, 1901-1936
  • UTC +1:30: Was used in present-day Nambia and parts of South Africa, 1892-1903
  • UTC +2:30: Was used in Moscow in late 19th century (now UTC +4:00 in winter)
  • UTC +4:51: Used as Bombay time (India) until 1951
  • UTC +7:20: Was used as daylight saving time in Singapore between 1933 and 1940
  • UTC +7:30: Used in Singapore before 1970 (now UTC +8:00)
  • UTC +8:30: Formerly used in north eastern China and South Korea
  • UTC +9:45: Unofficially used in Eucla and surrounds (Australia, see above) in summer when Western Australia had daylight saving

References

[1] Time zone (Wikipedia)

[2] List of time zones by UTC offset (Wikipedia)

January 30, 2013

Similar triangles fitting together in two ways

Filed under: mathematics — ckrao @ 11:58 am

In my previous mathematical post we observed that if three triangles fit together to form a triangle or quadrilateral, then they also can fit together in a second way. I thought this point was noteworthy enough to form a blog post of its own.

One of the examples from the previous post is reproduced below.

45-30-15-fittingequifitting

More generally, we have the following result.

Given points A, B, C, D in the plane there exist points P, Q, R, S in the plane so that

  • \displaystyle \triangle ABD \sim \triangle PQS
  • \displaystyle \triangle ACD \sim \triangle RQS
  • \displaystyle \triangle BCD \sim \triangle RPS

tri-fitting

To prove this, first construct \triangle PQS \sim ABD and choose R so that \triangle ACD \sim \triangle RQS and the triangles have the same orientation (i.e. vertices labelled in the same direction clockwise or anticlockwise). This can be done in one way only. We now wish to show that in this configuration we have the third condition \triangle BCD \sim \triangle RPS. We shall use complex number geometry to show this.

Let z_1 represent the spiral similarity that maps DA to DB.

Let z_2 represent the spiral similarity that maps DB to DC.

Let z_3 represent the spiral similarity that maps DC to DA.

Then the composition of these three maps is the identity so we have z_3 z_2 z_1 = 1. But since \triangle ABD \sim \triangle PQS, z_1 also maps SP to SQ. Similarly z_3 maps SQ to SR.

Therefore z_3z_1 = 1/z_2 maps SP to SR, or in other words z_2 maps SR to SP. This shows that \triangle BCD \sim \triangle RPS, as we wished to show.

It’s fascinating to me that non-trivial geometrical ideas can follow from the arithmetic of complex numbers (in this case, the simple fact that z_1 z_2 z_3 = z_2 z_3 z_1).

January 16, 2013

Australia’s recent heat wave

Filed under: climate and weather — ckrao @ 11:09 am

Australia has started 2013 with something like 10 of its first 11 days among the hottest 20 previously determined over some 100 years of records! The previous record area-averaged maximum of 40.17°C (set in December 1972) was broken on January 7 with 40.33°C. The two striking features of this heat wave have been its duration and wide-reaching nature. It included Hobart’s highest recorded maximum of 41.8°C and Australia’s hottest day for 15 years (49.6°C at Moomba, SA). Other very high temperatures included 49.0 at both Leonora (WA) and Birdsville (QLD).

The following graph based on data in [1] shows the maximum temperatures over the states and territories over this period. Note that the southern states of VIC and TAS are the smallest and have the least impact on the average temperature for Australia. For information on how area averages are calculated based on the weather station locations, refer to [2].

area-averaged

Birdsville probably was probably the hottest town in Australia over this period with the following maximum temperatures recorded (an average maximum of 45.6°C over the 13 days!). (Data from here).

Date
(Jan 2013)
Maximum Temp (°C)
1 43.9
2 45.2
3 45.5
4 47.3
5 46.7
6 46.3
7 45.1
8 44.6
9 44.2
10 40.8
11 46.2
12 48.6
13 49.0

References

[1] Extreme January heat: Special Climate Statement Issued 7th of January 2013, updated 25th January 2013, Bureau of Meterology, Australia.

[2] D. Jones, W. Wang and R. Fawcett, High-quality spatial climate data-sets for Australia, Australian Meteorological and Oceanographic Journal 58 (2009) 233-248.

January 6, 2013

Triangles on the sides of a triangle

Filed under: mathematics — ckrao @ 5:34 am

I have always enjoyed geometry results that are simple to state and elegant in nature. Napoleon’s theorem certainly qualifies.

If equilateral triangles are erected externally on the sides of any triangle, their centres form an equilateral triangle.

Interestingly, this result is also true for three points on a straight line.

Here is a similar problem, this time with different triangles on two of the sides.

Let A,B,C be three points in the plane. Construct an equilateral triangle EAC and a 120-30-30 triangle FAB (with \angle AFB = 120^{\circ}) both external to ABC. Let D be the midpoint of AB. Prove DEF is a 90-30-60 triangle.

Both this and the previous result can be proved using transformation geometry. We use the beautiful result that a rotation is the composition of two reflections, and this result allows us to compose two rotations about two different points.

A rotation of angle \theta about a point P is a composition of reflections in two lines, both through P, which have angle \theta/2 between them. The orientation of the two lines does not matter, only the relative angle between them. In the figure below the rotation is equivalent to a reflection in the line \ell followed by the line m, both through P.

two_lines

Now consider the problem of a rotation (anticlockwise) of angle \theta_1 about point P_1 followed by a second rotation of angle \theta_2 about point P_2. We replace each rotations as a pair of reflections through P_1 and P_2 respectively. Since only the angle between the lines matters (\theta_1/2 and \theta_2/2 respectively), we may assume one of the lines for each rotation to pass through both P_1 and P_2. Hence we have a total of three lines, say \ell, m, n shown below. Assume m passes through P_1P_2.

threelines

Now the composition of two rotations can be expressed as the composition of four reflections: firstly in lines \ell and m (corresponding to the first rotation) followed by lines m (again) and n. Since two successive reflections in the same line are equivalent to the identity transformation (i.e. back to the original configuration), the net effect of these four reflections is a reflection in the line \ell followed by a reflection in line n. This is equivalent to a rotation in the angle twice that between the two lines \ell and m, about the point Q where they intersect. By a simple angle chase, this rotation angle is found to be \theta_1 + \theta_2.

Applying this result to our 90-30-60 problem above, we consider the following two rotations:

  • about E with rotation angle 60 degrees
  • about F with rotation angle 120 degrees

Under the first rotation the point C maps to A. Under the second the point A maps to B. Hence the net effect is a rotation of (60 + 120) degrees that takes C to B. This rotation can only occur about the midpoint of BC, in other words about D. The centre of rotation is also found by joining E and F, forming lines that have angle 60/2 and 120/2 with EF, then finding their point of intersection. Overall a 30-60-90 triangle is formed and the centre of rotation is where the 90 degree angle occurs, as required.

One can try to prove Napoleon’s theorem in a similar way. The general result is as follows.

Given three points A, B, C in the plane construct isosceles triangles DBC, ECA, FAB so that \angle CDB = 2\alpha, AEC = 2\beta, BFA = 2\gamma where \alpha + \beta + \gamma =180^{\circ} and DB=DC, EC = EA, FA = FB. Then triangle DEF has angles independent of the positions of A,B,C and in fact \angle EDF = \alpha, \angle FED = \beta, \angle DFE = \gamma.

alpha-beta-gamma

The above results are special cases since 120 + 120 + 120 = 360 = 60 + 120 + 180. We can also allow for the case when any of the isosceles triangles are constructed internally, in which case the corresponding angles \alpha, \beta or \gamma are between -180^{\circ} and 0^{\circ}. (An angle of -\theta anticlockwise is simply equivalent to an angle of 360-\theta anticlockwise or \theta clockwise.) Then the above result almost holds when \alpha + \beta + \gamma =0^{\circ} or -180^{\circ} though in these cases one or more of the angles \angle EDF, \angle FED, \angle DFE may need to be adjusted by  180^{\circ} to ensure they sum to \pm 180^{\circ}.

In the following figure we chose \alpha = 60^{\circ}, \beta = \gamma = -30^{\circ}, leading to \angle EDF = 60-180=-120^{\circ}, \angle FED = \angle DFE = -30^{\circ} as shown.

120-30-30

An example from the IMO

Now let us look at an even more general case when the triangles erected on the sides of ABC are not necessarily isosceles. Consider the following example from the 1977 IMO. In the figure the triangle ABC is arbitrary and angles are as shown. We are required to show that  DE=DF and DE \perp DF.

IMO-75-3

This time we can proceed by considering spiral similarities (dilations composed with rotations) about B and C. Here we consider the composition of the following two spiral similarities.

  • 45^{\circ} about C, scale factor AC/EC mapping E to A
  • 45^{\circ} about B, scale factor FB/AB mapping A to F

The composition is a new spiral similarity mapping E to F. We use the fact now that the composition of two spiral similarities is a spiral similarity with dilation factor given by the product of the two scale factors and rotation angle the sum of the two rotation angles. We know that the dilation factor of the composition factor will be AC/EC \times FB/AB = 1 (by the similarity of triangles AEC and AFB) and the rotation angle will be 45^{\circ} + 45^{\circ} = 90^{\circ}. If we can prove the centre of this composition spiral similarity is D we are done since that would mean we now have a 90^{\circ} rotation mapping E to F.

To do this we show that D is fixed under the composite transformation. Let G be the point making \triangle BCG equilateral as shown below. Then by symmetry \angle CGD = \angle GBD = 60 - 15 = 45^{\circ} and \angle CGD = \angle BGD = 30^{\circ}. Under the first spiral similarity D will map to G (since \triangle DCG \sim \triangle ECA and under the second G will map back to D (since \triangle GBD\sim \triangle ABF). This proves that D is fixed under the composite transformation as required.

IMO-75-3-sol

Generalisation

Let us seek now to generalise this result. What is the relationship between the angles of the three triangles external on the side of an arbitrary triangle so that the three new vertices form a triangle independent of the angles of our original triangle? It is convenient to express our spiral similarities in terms of complex numbers.

Referring to the diagram above let the points A, B, C, D, E, F be represented by complex numbers a, b, c, d, e, f.

  • Let z_1 be the spiral similarity that maps DC to DB.
  • Let z_2 be the spiral similarity that maps EA to EC.
  • Let z_3 be the spiral similarity that maps FB to FA.

We may then write z_1 = (b-d)/(c-d) from which d = c - (b-c)/(z_1 - 1) = c - w_1(b-c) where for convenience we let w_i = 1/(z_i - 1) for i = 1,2,3. Similarly e = a - w_2(c-a) and f = b - w_3(a - b).

We would like the shape of \triangle DEF to be independent of ABC. In complex numbers one way of expressing this is to say the ratio (f-d)/(e-d) is independent of a, b, c. In other words there is some complex number \alpha (w_1, w_2, w_3) independent of a,b,c such that

\displaystyle \alpha (w_1, w_2, w_3) := \frac{f-d}{e-d} = \frac{a(-w_3) + b(1 + w_3 + w_1) + c(-1 - w_1)}{a(1 + w_2) + b w_1 + c(-w_2 - 1 - w_1)}.

Assuming non-zero denominators this leads to

\displaystyle \alpha = \frac{-w_3}{1 + w_2} = \frac{1 + w_3 + w_1}{w_1} = \frac{1+w_1}{w_2 + 1 + w_1}.

Equality of the first and third w_i expressions implies

\displaystyle w_3 = \frac{-(1 + w_2)(1 + w_1)}{1 + w_1 + w_2}.

(Note that the middle w_i expression follows from the other two by addendo and so need not be used.) The above can be rearranged as

\displaystyle 1 + \frac{1}{w_3} = \frac{-(1 + w_1 + w_2)}{(1 + w_1)(1 + w_2)} +1 = \frac{w_1w_2}{(1 + w_1)(1 + w_2)}.

Recalling that w_i = 1/(z_i - 1), this implies (w_i + 1)/w_i = 1 + 1/w_i = z_i, so the above may be written in the attractive form

\displaystyle z_1 z_2 z_3 = 1.

This form is expected since it corresponds to the product of the three spiral similarities about the point D in the above figure:

  • Spiral similarity z_3 maps DB to DG
  • Spiral similarity z_2 maps DG to DC
  • Spiral similarity z_1 maps DC to DB

Another way of interpreting the equality z_1 z_2 z_3 = 1 is that the sum of the apex angles \angle CDB, \angle AEC, \angle BFA is an integer multiple of 360^{\circ} and

\displaystyle \frac{DB}{DC} \cdot \frac{EC}{EA} \cdot \frac{FA}{FB} = 1.

A consequence of this relationship is that the three triangles external to the original triangle may be scaled so that they “fit together” as seen above when forming the triangle BCG. The triangles fit together in a second way to form the shape of DEF, shown below.

45-30-15-fitting

The following shows how the triangles fit together in the -60,-60,120 case we considered earlier.

bluegreenredfitting

Note that in this case the triangles fit together to form a quadrilateral.

In general the angles of the new triangle are related to the original three triangles via the following figure (here the case of triangles erected externally is shown).

general_angles

If we start with a configuration of any four points in the plane we may construct our triangles in the following way, rephrasing the z_1z_2 z_3 = 1 result.

Let P,Q,R,S be points in the plane and A,B,C three other points. Construct points D, E, F so that \triangle BCD \sim \triangle SQR, \triangle ACE \sim \triangle SPR and \triangle ABF \sim \triangle QPR. Then \triangle DEF has angles independent of \triangle ABC.

Another statement of this is the following found in [1].

If similar triangles ADB, CBE and FAC are erected outwardly on the sides of any triangle ABC, and any three points P, Q and R are chosen so that they respectively lie in the same relative positions to these triangles, then P, Q and R form a triangle similar to the three triangles.

For me the beauty of these results comes from the fact that the angles of the triangles are not related through any obvious chasing of angles – additional insights are necessary.

Reference

[1] Curious triangle fact – posted in geometry.pre-college forum in Nov 1995.

Create a free website or blog at WordPress.com.

%d bloggers like this: