Not exact matches
If the researchers incorrectly estimated a 200,000 - year - old salamander species to be 2 million years old,
then their result was off by a factor of 10, making the salamander's rate of evolution 20,000 times
slower than
climate change instead of 200,000 times
slower.
Once the ice reaches the equator, the equilibrium
climate is significantly colder than what would initiate melting at the equator, but if CO2 from geologic emissions build up (they would, but very slowly — geochemical processes provide a negative feedback by
changing atmospheric CO2 in response to
climate changes, but this is generally very
slow, and thus can not prevent faster
changes from faster external forcings) enough, it can initiate melting — what happens
then is a runaway in the opposite direction (until the ice is completely gone — the extreme warmth and CO2 amount at that point, combined with left - over glacial debris available for chemical weathering, will draw CO2 out of the atmosphere, possibly allowing some ice to return).
Most
climate change predictions, when they incorporate population growth at all, have been based on the long - standing assumption that the planet's burden of humans will peak around 2050, and
then begin a
slow decline.
Human - induced forcing exhibited a
slow rise during the early part of the last century but
then accelerated after 1960.2 Thus, these graphs highlight observed
changes in
climate during the period of rapid increase in human - caused forcing and also reveal how well
climate models simulate these observed
changes.
If MJ's death motivated to you spend 4 minutes listening to song you wouldn't have listened to last week,
then email your Senators and tell them the
climate change bill before them is far too weak and too
slow.
A new assessment by the Intergovernmental Panel on
Climate Change (IPCC) concludes that the world community could
slow and
then reduce global emissions of greenhouse gases (GHGs) over the next several decades by exploiting cost - effective policies and current and emerging technologies.
But concrete action to address
climate threats has been relatively slow, critics say, and a convoluted process of devolution of power to Pakistan's provinces and then the reorganisation of federal ministries hasn't helped speed up the process — though a new federal Ministry of Climate Change may help chang
climate threats has been relatively
slow, critics say, and a convoluted process of devolution of power to Pakistan's provinces and
then the reorganisation of federal ministries hasn't helped speed up the process — though a new federal Ministry of
Climate Change may help chang
Climate Change may help change
Change may help
changechange that.
Slowing the growth rate of GHG emissions and
then reversing it is the key to addressing
climate change and keeping global average temperature below 2 °C above pre-industrial levels.
Glacial — interglacial oscillations of the CO2 amount and ice sheet size are both
slow climate feedbacks, because glacial — interglacial
climate oscillations largely are instigated by insolation
changes as the Earth's orbit and tilt of its spin axis
change, with the
climate change then amplified by a nearly coincident
change of the CO2 amount and the surface albedo.