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Space Weather Radiation Hazards REU Summer School. By Ron Zwickl NOAA Space Environment Center June 14, 2007. Space Weather Radiation Hazards Outline. Simple Tutorial Cosmic Rays Solar Radiation Storms Earth’s Influence Magnetospheric Shielding Atmospheric Shielding
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Space Weather Radiation Hazards REU Summer School By Ron Zwickl NOAA Space Environment Center June 14, 2007
Space Weather Radiation Hazards Outline • Simple Tutorial • Cosmic Rays • Solar Radiation Storms • Earth’s Influence • Magnetospheric Shielding • Atmospheric Shielding • Radiation Impacts on Airline Passengers • Radiation Dangers to Astronauts REU Summer School
Space Radiation • Composed of two major components • Cosmic Rays • Always present and very energetic • Composed of many different elements REU Summer School
Cosmic Rays are “born” throughout the known Universe
Cosmic Rays • Composed of many • different Elements, • such as Hydrogen • Helium, Carbon, and Iron • They cover a very wide • range of energies • They are always present REU Summer School
GALACTIC COSMIC RAYS REU Summer School
Space Radiation • Composed of two major components • Cosmic Rays • Always present and very energetic • Composed of many different elements • Intensity varies throughout 11 year Solar Cycle REU Summer School
Radiation level varies throughout the solar cycle REU Summer School
Space Radiation • Composed of two major components • Cosmic Rays • Always present and very energetic • Composed of many different elements • Intensity varies throughout 11 year Solar Cycle • Intensity varies with Solar Activity REU Summer School
Space Radiation • Composed of two major components • Cosmic Rays • Always present and very energetic • Composed of many different elements • Intensity varies throughout 11 year Solar Cycle • Intensity varies with Solar Activity • Solar Radiation Storms • Infrequent, very intense, with rapid onsets REU Summer School
Flight crews Interested in this curve S4 Solar Radiation Storm S3 S2 S1 REU Summer School
Polar Satellite Image Degradation during July 14, 2000 Solar Radiation Storm
Space Radiation • Composed of two major components • Cosmic Rays • Always present and very energetic • Composed of many different elements • Intensity varies throughout 11 year Solar Cycle • Intensity varies with Solar Activity • Solar Radiation Storms • Infrequent, very intense, with rapid onsets • Composed of many different elements • Origin strongly linked to Solar Activity • Variable energy and composition dependence REU Summer School
Space Radiation • Earth’s Influence on the radiation level • Magnetic Field Shielding • Always present, but has holes! REU Summer School
Open Closed Open Cosmic Ray Access REU Summer School
Earth’s Magnetic Shield to Cosmic Ray Access Magnetic Poles: Open Magnetic Equator: >15 GeV Red bar varies as function of magnetic latitude REU Summer School
Space Radiation • Earth’s Influence on the radiation level • Magnetic Field Shielding • Always present, but has holes! • Geomagnetic Activity • Changes magnetic field shield location REU Summer School
Influence of Geomagnetic Activity on auroral boundary (geomagnetic poles expand with increased activity)
Space Radiation • Earth’s Influence on the radiation level • Magnetic Field Shielding • Always present, but has holes! • Geomagnetic Activity • Changes magnetic field shield location • Atmospheric Shielding • Upper atmosphere acts as a target • Lower atmosphere acts as absorbing shield REU Summer School
Photon cascade in lead plates in cloud chamber. Maximum number of particles after passing through 10 cm of lead Incident photon is several GeV
Space RadiationSummary • Two primary components • Cosmic Rays • Steady with some variability • Solar Radiation Storms • Rare, highly variable, and can be intense • Earth’s natural defenses • Magnetic field shields Earth • Makes calculations very complex • Geomagnetic Latitude dependent • Geomagnetic activity can expand poles • Atmosphere acts as target and as shield • Radiation strongly dependent upon altitude REU Summer School
Space Weather and Aviation REU Summer School
FRA to DFW flight REU Summer School
Slide 7 Issue Time: 2001 Nov 04 2045 UTC ALERT: Solar Radiation Alert at Aviation Flight Altitudes Conditions Began: 2001 Nov 04 2035 UTC Altitude Solar proton effective dose rate (feet) (millisieverts/hour) * --------------------------------------------------------------- 20 000 <0.0010 30 000 0.0052 40 000 0.019 50 000 0.040 60 000 0.060 70 000 0.074 80 000 0.088 ---------------------------------------------------------------- * Estimates at high latitude locations. Dose rates are based on near real-time GOES satellite readings and are recalculated every 3 minutes. REU Summer School Kyle Copeland & Wallace Friedberg Civil Aerospace Medical Institute, AAM-610
Space Weather and Aviation REU Summer School
Slide 9 Effective Doses From Solar Radiation at 40 000 ft for Selected Solar Proton Events From January 1986 Through December 2001 (16 y) Total Effective Dose (mSv) ----------------------------- Date Event Time (hh:mm)* 3 h 5 h 10 h ---------------------------------------------------------------------------------- Aug. 16, 1989 GLE 41 01:10 0.055 0.072 0.087 Sept. 29, 1989** GLE 42 08:35 0.26 0.42 0.59 Oct. 19, 1989 GLE 43 20:30 0.074 0.17 0.41 Oct. 22, 1989 GLE 44 03:25 0.15 0.19 0.23 Oct. 24, 1989 GLE 45 10:25 0.14 0.37 0.64 May 24, 1990 GLE 48 00:05 0.13 0.019 0.026 Jun. 15, 1991 GLE 52 00:50 0.041 0.048 0.055 Nov. 2, 1992 GLE 54 00:20 0.039 0.054 0.072 Nov. 6, 1997** GLE 55 08:00 0.15 0.26 0.39 Jul. 14, 2000** GLE 59 07:05 1.1 1.3 1.51 Apr. 15, 2001** GLE 60 07:35 0.73 0.97 1.1 Apr. 18, 2001** GLE 61 01:15 0.049 0.083 0.14 Nov. 4, 2001** GLE 62 03:20 0.082 0.12 0.17 Dec. 26, 2001 GLE 63 01:35 0.069 0.081 0.090 ---------------------------------------------------------------------------------- * Time that recommended maximum flight altitude is below 40 000 ft ** Dose rates are underestimated for more than 0.5 h REU Summer School Kyle Copeland & Wallace Friedberg Civil Aerospace Medical Institute, AAM-610
Radiation Risks to Astronauts NASA routinely avoids the radiation belts in their scheduling of space walks. Michael J. Golightly
DEEP SPACE GCR DOSES • Annual bone marrow GCR doses will range up to ~ 15 cGy at solar minimum (~ 40 cSv) behind ~ 2cm Al shielding • Effective dose at solar minimum is ~ 45-50 cSv per annum • At solar maximum these are ~ 15-18 cSv • Secondary neutrons and charged particles are the major sources of radiation exposure in an interplanetary spacecraft • No dose limits yet for these missions REU Summer School
GCR Risks • Clearly, annual doses < 20cGy present no acute health hazard to crews on deep space missions • Hence only stochastic effects such as cancer induction and mortality or late deterministic effects, such as cataracts or damage to the central nervous system are of concern. • Unfortunately, there are no data for human exposures from these radiations that can be used to estimate risks to crews • In fact, it is not clear that the usual methods of estimating risk by calculating dose equivalent are even appropriate for these particles REU Summer School
SOLAR PARTICLE EVENT DOSES • Doses can be large in deep space but shielding is possible • August 1972 was largest dose event of space era (occurred between two Apollo missions) REU Summer School
POSSIBLE ACUTE EFFECTSAugust 1972 SPE • Bone marrow doses ~ 1 Gy delivered in a day may produce hematological responses and vomiting (not good in a space suit) • Skin doses ~15-20 Gy could result in skin erythema and moist desquamation (in some cases) - doses inside nominal spacecraft might limit effects to mild erythema REU Summer School
SOLAR PARTICLE EVENT DOSES • Ice core data from the Antarctic indicate that the largest event in past ~ 500 years was probably the Carrington Flare of 1859 - fluence ~ 20 larger than Aug 72 - actual spectrum energy dependence unavailable, assume both hard and soft spectra REU Summer School
CARRINGTON FLARE DOSES(9/89 Spectrum) • Bone marrow doses ~ 1-3 Gy possible inside a spacecraft (life threatening) • “Storm” shelter of about 18 cm Al needed to shield to the applicable deterministic limits (30 d limits of 0.25 Gy-Eq) • Major problem for non radiation hardened electronics built with COTS components - up to 50 krads or more of total ionizing dose REU Summer School
Mars Surface(mainly protons and neutrons) REU Summer School
CONCLUDING REMARKS • GCR exposures will be a problem for Mars missions due to large effective doses • Organ doses received from large SPEs can be hazardous to crews of vehicles in deep space - exposures that are survivable with proper medical treatment on Earth may not be survivable in space REU Summer School
CONCLUDING REMARKS (cont.) • Aside from acute effects, a single large SPE can expose a crewmember to an effective dose that exceeds their career limit • Due to their relatively soft energy spectra, most SPE doses can be substantially reduced with adequate shielding (several cmAl or equivalent) • A worst case event similar to the assumed Carrington Flare of 1859 could be catastrophic in deep space depending on spectral hardness REU Summer School
CONCLUDING REMARKS (cont.) • Results presented only for aluminum • Other materials with low atomic mass numbers are better LH2 reduces GCR dose equivalent by ~ one-half • In situ materials on lunar or Martian surface can be used to provide shielding (similar to Al in shielding characteristics) • Martian atmosphere is a relatively thick shield for operations on Mars surface ~ 16-20 g cm-2 CO2 REU Summer School
parting shot … Kanzelhoehe Solar Observatory, Austria December 1, 2000
October 1989 SPE REU Summer School
AUGUST 1972 SKIN DOSE RATE REU Summer School
UAL POLAR ROUTES NEW YORK 82 N CHICAGO #1 #1A #2 #3 #4 BEIJING SHANGHAI HONG KONG OSAKA TOKYO REU Summer School