http://www.lpl.arizona.edu/impacteffects/
http://en.wikipedia.org/wiki/99942_Apophis
The site is a calculator for the effects of an asteroid hitting us. Just find data on Apophis and plug it in.
Update:
I did a bit of the work here, and found some data. Credit goes to the site and wikipedia.
Impact Effects
Robert Marcus, H. Jay Melosh, and Gareth Collins
Please note: the results below are estimates based on current (limited) understanding of the impact process and come with large uncertainties; they should be used with caution, particularly in the case of peculiar input parameters. All values are given to three significant figures but this does not reflect the precision of the estimate. For more information about the uncertainty associated with our calculations and a full discussion of this program, please refer to this article
Your Inputs:
Distance from Impact: 80.50 km = 49.99 miles
Projectile Diameter: 250.00 m = 820.00 ft = 0.16 miles
Projectile Density: 1500 kg/m3
Impact Velocity: 30.73 km/s = 19.08 miles/s
Impact Angle: 45 degrees
Target Density: 2750 kg/m3
Target Type: Crystalline Rock
Energy:
Energy before atmospheric entry: 5.79 x 1018 Joules = 1.38 x 10^3 MegaTons TNT
The average interval between impacts of this size somewhere on Earth during the last 4 billion years is 2.9 x 104years
Atmospheric Entry:
The projectile begins to breakup at an altitude of 82000 meters = 269000 ft
The projectile reaches the ground in a broken condition. The mass of projectile strikes the surface at velocity 23 km/s = 14.3 miles/s
The impact energy is 3.25 x 1018 Joules = 7.77 x 10^2MegaTons.
The broken projectile fragments strike the ground in an ellipse of dimension 1.21 km by 0.859 km
Major Global Changes:
The Earth is not strongly disturbed by the impact and loses negligible mass.
The impact does not make a noticeable change in the Earth's rotation period or the tilt of its axis.
The impact does not shift the Earth's orbit noticeably.
Crater Dimensions:
What does this mean? Crater shape is normal in spite of atmospheric crushing; fragments are not significantly dispersed.
Transient Crater Diameter: 3.15 km = 1.96 miles
Transient Crater Depth: 1.12 km = 0.692 miles
Final Crater Diameter: 3.68 km = 2.29 miles
Final Crater Depth: 0.438 km = 0.272 miles
The crater formed is a complex crater.
The volume of the target melted or vaporized is 0.0205 km^3 = 0.00491 miles3
Roughly half the melt remains in the crater
Thermal Radiation:
What does this mean? Time for maximum radiation: 0.129 seconds after impact
Visible fireball radius: 2.46 km = 1.52 miles
The fireball appears 6.93 times larger than the sun
Thermal Exposure: 1.88 x 105 Joules/m2
Duration of Irradiation: 38.5 seconds
Radiant flux (relative to the sun): 4.87 Seismic Effects:
What does this mean? The major seismic shaking will arrive at approximately 16.1 seconds.
Richter Scale Magnitude: 6.5
Mercalli Scale Intensity at a distance of 80.5 km:
IV. Felt indoors by many, outdoors by few during the day. At night, some awakened. Dishes, windows, doors disturbed; walls make cracking sound. Sensation like heavy truck striking building. Standing motor cars rocked noticeably.
V. Felt by nearly everyone; many awakened. Some dishes, windows broken. Unstable objects overturned. Pendulum clocks may stop. Ejecta:
What does this mean? The ejecta will arrive approximately 129 seconds after the impact.
At your position the ejecta arrives in scattered fragments
Average Ejecta Thickness: 1.69 mm = 0.0666 inches
Mean Fragment Diameter: 4.01 cm = 1.58 inches Air Blast:
What does this mean? The air blast will arrive at approximately 244 seconds.
Peak Overpressure: 10600 Pa = 0.106 bars = 1.51 psi
Max wind velocity: 24 m/s = 53.7 mph
Sound Intensity: 81 dB (Loud as heavy traffic)
Damage Description: Glass windows will shatter.
Tell me more...
Click here for a pdf document that details the observations, assumptions, and equations upon which this program is based. It describes our approach to quantifying the important impact processes that might affect the people, buildings, and landscape in the vicinity of an impact event and discusses the uncertainty in our predictions. The processes included are: atmospheric entry, impact crater formation, fireball expansion and thermal radiation, ejecta deposition, seismic shaking, and the propagation of the atmospheric blast wave.
Earth Impact Effects Program Copyright 2004, Robert Marcus, H.J. Melosh, and G.S. Collins
These results come with ABSOLUTELY NO WARRANTY