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Where is the best site on Earth?<br />

<strong>Dome</strong>s A, B, C and F,<br />

and Ridges A and B<br />

Will Saunders 1,2 , Jon Lawrence 1,2,3 , John Storey 1 , Michael<br />

Ashley 1 , Seiji Kato 4 , Pat Minnis 4 , David Winker 4 , Guiping Liu 5<br />

1 University of New South Wales. 2 Anglo-Australian Australian Observatory.<br />

3 Macquarie University. 4 NASA Langley Research Center.<br />

5 Space Sciences Lab, University of California Berkeley.<br />

PASP, almost in press


Site comparison includes<br />

Boundary layer thickness<br />

Cloud cover<br />

Auroral emission<br />

Airglow<br />

Atmospheric thermal backgrounds<br />

Precipitable water vapour (PWV)<br />

Telescope thermal backgrounds<br />

Free atmospheric seeing<br />

Doesn't include<br />

Non-winter use<br />

Sky coverage<br />

Dark time<br />

Infrastructure<br />

Non-astronomical uses<br />

F<br />

A<br />

C<br />

B


•F<br />

•A<br />

•G<br />

B<br />

•C<br />

Site Latitude Longitude Elevation Λ(2010)<br />

<strong>Dome</strong> A 80.37S 77.53E 4083m -84.9°<br />

<strong>Dome</strong> C 75.06S 123.23E 3233m -84.1°<br />

<strong>Dome</strong> F 77.19S 39.42E 3810m -77.0°<br />

Ridge B 76-79°S 97-93°E 3700-3809m -85.4° -87.1°<br />

South Pole 90°S 0°E 2800m -80.0°


BOUNDARY LAYER<br />

Swain & Gallee 2006a, 2006b;<br />

van Lipzig 2004, Parish & Bromwich 2007<br />

• Thinnest along<br />

'katabatic ridge'<br />

<strong>Dome</strong> A – Ridge B<br />

• + <strong>Dome</strong> F, <strong>Dome</strong> C<br />

• <strong>Dome</strong> F is best<br />

• <strong>Dome</strong> A is not quite<br />

on katabatic ridge


CLOUD COVER<br />

Aqua/MODIS satellite data, validated against GLAS, also CALIPSO<br />

Spring<br />

Summer<br />

Autumn<br />

Winter<br />

• Best weather<br />

along <strong>Dome</strong> F –<br />

<strong>Dome</strong> A – Ridge<br />

B – <strong>Dome</strong> C<br />

• Best weather<br />

misses <strong>Dome</strong> A<br />

• <strong>Dome</strong> C has best<br />

weather?


AURORAE<br />

Dempsey et al 2005 results for <strong>Dome</strong> C incorrect<br />

Used Hardy 1991 models, + South Pole<br />

measurements from Dempsey et al 2005<br />

Site Λ (2010)<br />

South Pole -80°<br />

<strong>Dome</strong> A -84.9°<br />

<strong>Dome</strong> C -84.1°<br />

<strong>Dome</strong> F -77.0°<br />

Ridge B -85.4° -<br />

87.1°<br />

• <strong>Dome</strong> A, <strong>Dome</strong> C,<br />

Ridge B very similar<br />

• Not much dependence<br />

on solar activity level,<br />

but brightest at solar<br />

minimum<br />

• 20-30% increase at V,<br />

100% at B<br />

• <strong>Dome</strong> F much worse


AIRGLOW<br />

From models of Liu et al 2008<br />

OI + OH<br />

Validated only for |latitude| < 40°<br />

Not much dependence on local time<br />

OI<br />

OH<br />

• OI much worse ( x 5) than<br />

temperate sites<br />

• OH ~25% worse<br />

• Spring OH hole,<br />

only <strong>Dome</strong> C can use


FREE ATMOSPERIC SEEING<br />

• Data from NCAR/NCEP reanalysis, May-Aug, 1995 - 2008<br />

• Use standard relations to get<br />

C n<br />

2<br />

= 3.62 x 10 -5 (P g) -2/3 (1/θ dθ/dz |dV/dz| ) 4/3<br />

• Assume |dV/dz| ∝ V<br />

(i.e. profiles are self-similar)<br />

• Use Trinquet et al (2008)<br />

profile as template<br />

⇒ C n2 profile at all positions


-60°<br />

-75°<br />

Seeing<br />

FREE ATMOSPHERIC SEEING cont.<br />

• Best between SP and DA<br />

• <strong>Dome</strong> F very good<br />

• large factors (x10!) in 'coherence volume'<br />

• Predicts South Pole better than <strong>Dome</strong> C ?<br />

• Very crude model, can do better!<br />

Isoplanatic angle<br />

Site ε 0<br />

(") θ 0<br />

(") τ 0<br />

(ms)<br />

South Pole 0.19 5.43 18.8<br />

<strong>Dome</strong> A 0.22 5.57 16.0<br />

Ridge A 0.21 6.29 17.6<br />

<strong>Dome</strong> C 0.26 3.39 8.44<br />

<strong>Dome</strong> F 0.21 5.17 15.4<br />

Coherence time<br />

Ridge B 0.23 4.07 11.1


ATMOSPHERIC THERMAL EMISSION<br />

Temperature data from NCAR/NCEP reanalysis<br />

Colder site ⇒ wider K dark<br />

Coldest between South Pole and<br />

<strong>Dome</strong> A<br />

Only measurement of K dark<br />

is at SP<br />

Origin of K dark<br />

background unknown<br />

Factors of 1.5-2 in thermal IR<br />

background between sites<br />

(Lawrence 2004)<br />

10000<br />

1000<br />

100<br />

Sky Brightness (Jy.arcsec -2 )<br />

10<br />

1<br />

0.1<br />

0.01<br />

1E-3<br />

1E-4<br />

1E-5<br />

1E-6<br />

3 4 5 6 7 8 9 10 11 12 13 14 15<br />

W avelength (μm)


PRECIPITABLE WATER VAPOUR<br />

Prediction from Swain and Gallee 2006b<br />

Should have real data from MHS sensor<br />

on NOAA-18 satellite.<br />

• Factor of 2 variations<br />

• Best between South Pole<br />

and <strong>Dome</strong> A<br />

• <strong>Dome</strong> F almost as good<br />

• <strong>Dome</strong> C not so good


SURFACE TEMPERATURE<br />

Prediction from Swain and Gallee 2006b<br />

Measurement from MODIS on Aqua satellite<br />

Variations quite small (few °)<br />

<strong>Dome</strong> A 204.1<br />

<strong>Dome</strong> C 204.9<br />

<strong>Dome</strong> F 204.9<br />

Ridge B 203.6<br />

<strong>Dome</strong> B 206.9<br />

Ridge A 203.5


DOME A versus 'RIDGE A'<br />

• Boundary layer, weather, free atmospheric seeing, atmospheric<br />

thermal emission, PWV, surface temperature ALL favour a site<br />

nearer South Pole<br />

• Obvious candidate is at the end of 'Ridge A' at (81.5°S 73.5°E 4053m)<br />

•RA<br />

•DA


'SUMMARY TABLE'<br />

SP DA RB DC DF RA<br />

Cloud Cover × √ √√ √√√ √√ √√<br />

Boundary Layer × √ √√ √ √√√ √√<br />

Aurorae × √ √ √ ×× √<br />

Free seeing √√√ √√ √ √ √√√ √√√<br />

IR sky brightness/PWV √ √√√ √√ √ √√√ √√√<br />

Surface temperature × √√√ √√√ √√ √√ √√√


• The coldest surface temperatures are found along <strong>Dome</strong> F – <strong>Dome</strong> A – Ridge B<br />

– <strong>Dome</strong> C. But offset from topographic ridgeline.<br />

• The best winter weather is found along the same line, with same offset. <strong>Dome</strong> C<br />

may have the best weather.<br />

• Thinnest boundary layer is found at <strong>Dome</strong> F, <strong>Dome</strong> A, along Ridge B, and at<br />

<strong>Dome</strong> C, in that order. Again there is an offset from the topographic ridge.<br />

• Best expected free seeing, isoplanatic angle, coherence time is found between<br />

<strong>Dome</strong> A, <strong>Dome</strong> F and the South Pole.<br />

• The lowest wintertime atmospheric thermal emission, and the lowest<br />

precipitable water vapour, is also found between <strong>Dome</strong> A, <strong>Dome</strong> F and the<br />

South Pole.<br />

• <strong>Dome</strong>s A and C and Ridge B are all similar from an auroral point of view, with<br />

significant contribution to the optical sky brightness. <strong>Dome</strong> F is much worse.<br />

• Airglow is significantly brighter than for temperate sites, except possibly in the<br />

spring, when there is an 'OH hole'. <strong>Dome</strong> C is the only site able to use this<br />

opportunity.<br />

• <strong>Dome</strong> A is clearly the best existing site. ’Ridge A’ (~150km southwest of <strong>Dome</strong><br />

A ), is likely to be even better.<br />

• <strong>Dome</strong> F is a superb site, with the exception of auroral activity.<br />

• The peak of Ridge B is a very good site but without any unique advantages.<br />

• <strong>Dome</strong> C may be almost as good as any other site for 2.5m K<br />

use.

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