View Single Post
Old 09-27-2006, 07:55 PM   #32 (permalink)
Ch'i
Artist of Life
 
Ch'i's Avatar
 
Quote:
Originally Posted by Paradise Lost
If this is true, I'd like to how or why. The sun didn't just get warmer, so this would obviously something to look into to see if it has any connection to problems global warming might have caused, and therefore, caused the sun to have a more direct effect on us.
As I understand it, the sun cools down, and heats up regularly,. Though overrall it is on a cooling trend.

More evidence for man's impact on the environment...
Quote:
NOAA 2006-025
NOAA Public Affairs
FOR IMMEDIATE RELEASE
Contact: Jana Goldman
2/27/06


RESEARCHERS IDENTIFY CAUSES OF 1979-2003
UNUSUAL STEP-LIKE COOLING OF GLOBAL LOWER STRATOSPHERE

Findings from satellite observations combined with a new NOAA computer model show that a significant cooling of the global lower stratosphere between 1979 and 2003 occurred in steps. Research published this week finds that while human influences led to the overall cooling during the period, natural factors helped modulate the evolution of the cooling.

“This research advances our knowledge of fundamental influences, such as the role of greenhouse gases and volcanic eruptions, that force changes in the Earth's climate,” said Venkatachalam Ramaswamy, senior scientist at NOAA’s Geophysical Fluid Dynamics Laboratory in Princeton, N.J., and lead author of the paper. “The findings, derived from combining observations and numerical modeling studies, improves our understanding of how human and natural forcings cause changes in the Earth's climate system.”

The lower stratosphere is the region of the Earth's atmosphere from about 8 to 14 miles above the surface, where ozone plays a critical role in absorbing harmful ultraviolet radiation from the sun. Microwave Sounding Unit data from NOAA's polar orbiting satellites have shown that the two major volcanic eruptions, El Chichon in 1982 and Pinatubo in 1991, were initially followed by brief warming periods, then later by prolonged cooling periods in the global lower stratosphere.

“The unusual manner in which the cooling of the lower stratosphere evolved between 1979 and 2003 is very likely unique and unprecedented, and has not previously been well understood,” Ramaswamy said. “Climate model simulations show that human influences, namely stratospheric ozone depletion and greenhouse gas increases, and natural factors, namely volcanic aerosols and variations in the sun's energy output, combined to produce two step-like decreases in the lower stratospheric temperatures, one in the 1980s and the other in the 1990s.”

The simulations successfully replicated the complex observed stages of this temperature change, including the two step-like features marking the transitions of the lower stratosphere to a progressively colder state.

The simulations used a state-of-the-art coupled atmosphere-ocean model, developed at GFDL, one of NOAA's Office of Oceanic and Atmospheric Research laboratories. This laboratory has performed world-leading research in climate modeling for more than 50 years. The numerical calculations were performed on the NOAA supercomputer located at GFDL. The results of this research were carried out by a team that included scientists from GFDL, the National Center for Atmospheric Research, Lawrence Livermore National Laboratory, University of Miami and Rutgers University.

The researchers performed a variety of simulations employing combinations of the known changes in various factors, including human-made factors such as ozone depletion and long-lived greenhouse gas increases, and natural mechanisms of climate variability to see how these factors affected the cooling trend. The research indicates that the evolution of the cooling during 1979-2003 results from unusual juxtaposition of human-induced factors, volcanic events and the variations in the sun's output.

If ozone depletion continues, it would be an even more dominant factor in further lowering the stratospheric temperatures in the future. If there is complete ozone recovery because of the phasing out of the ozone-depleting substances, the stratospheric cooling trend would be governed by the long-lived greenhouse gases (e.g., CO2). Variations in the sun's output and any potential volcanic activity could affect the pattern. The findings are in a paper titled “Anthropogenic and Natural Influences in the Evolution of Lower Stratospheric Cooling” which was published in this week’s Science magazine.

The National Oceanic and Atmospheric Administration, an agency of the U.S. Commerce Department, is dedicated to enhancing economic security and national safety through the prediction and research of weather and climate-related events and providing environmental stewardship of our nation's coastal and marine resources. Through the emerging Global Earth Observation System of Systems (GEOSS), NOAA is working with its federal partners and 60 countries to develop a global monitoring network that is as integrated as the planet it observes.

Last edited by Ch'i; 09-27-2006 at 08:18 PM..
Ch'i is offline  
 

1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 25 26 27 28 29 30 31 32 33 34 35 36 37 38 39 40 41 42 43 44 45 46 47 48 49 50 51 52 53 54 55 56 57 58 59 60 61 62 63 64 65 66 67 68 69 70 71 72 73 74 75 76 77 78 79 80 81 82 83 84 85 86 87 88 89 90 91 92 93 94 95 96 97 98 99 100 101 102 103 104 105 106 107 108 109 110 111 112 113 114 115 116 117 118 119 120 121 122 123 124 125 126 127 128 129 130 131 132 133 134 135 136 137 138 139 140 141 142 143 144 145 146 147 148 149 150 151 152 153 154 155 156 157 158 159 160 161 162 163 164 165 166 167 168 169 170 171 172 173 174 175 176 177 178 179 180 181 182 183 184 185 186 187 188 189 190 191 192 193 194 195 196 197 198 199 200 201 202 203 204 205 206 207 208 209 210 211 212 213 214 215 216 217 218 219 220 221 222 223 224 225 226 227 228 229 230 231 232 233 234 235 236 237 238 239 240 241 242 243 244 245 246 247 248 249 250 251 252 253 254 255 256 257 258 259 260 261 262 263 264 265 266 267 268 269 270 271 272 273 274 275 276 277 278 279 280 281 282 283 284 285 286 287 288 289 290 291 292 293 294 295 296 297 298 299 300 301 302 303 304 305 306 307 308 309 310 311 312 313 314 315 316 317 318 319 320 321 322 323 324 325 326 327 328 329 330 331 332 333 334 335 336 337 338 339 340 341 342 343 344 345 346 347 348 349 350 351 352 353 354 355 356 357 358 359 360