Wildfires in Indonesia have been known to release massive amounts of carbon into
the atmosphere over short periods of time.
This could be random variation of
the atmosphere over a short period, or random measurement error, or some combination.
Not exact matches
Bowen and colleagues report that carbonate or limestone nodules in Wyoming sediment cores show the global warming episode 55.5 million to 55.3 million years ago involved the average annual release of a minimum of 0.9 petagrams (1.98 trillion pounds) of carbon to the
atmosphere, and probably much more
over shorter periods.
Scientists now think that massive volcanic activity, in a Large Igneous Province called the Siberian Traps, raised air and sea temperatures and released toxic amounts of greenhouse gases into the
atmosphere over a very
short period of time.
Methane has a relatively
short life in the
atmosphere where it oxidizes into CO2
over a
period of 9 - 15 years.
GHG continue to increase in amounts in the
atmosphere and as such,
over time more warming inevitably continues though there may be breaks for
short periods, and some cooling, as already discussed at great length regarding aerosols.
Methane has a relatively
short life in the
atmosphere where it oxidizes into CO2
over a
period of 9 — 15 years.
Despite this higher cumulative total, the green curve has a higher peak warming than the yellow curve because its emissions are put into the
atmosphere over a
shorter time
period.
This time
period is too
short to signify a change in the warming trend, as climate trends are measured
over periods of decades, not years.12, 29,30,31,32 Such decade - long slowdowns or even reversals in trend have occurred before in the global instrumental record (for example, 1900 - 1910 and 1940 - 1950; see Figure 2.2), including three decade - long
periods since 1970, each followed by a sharp temperature rise.33 Nonetheless, satellite and ocean observations indicate that the Earth -
atmosphere climate system has continued to gain heat energy.34
The
short - term change in surface temperature
over the 2000 - 2010
period is a result of ocean heat being exchanged with the
atmosphere (via ENSO).
«A reduction in the rate of warming (not a pause) is a result of
short - term natural variability, ocean absorption of heat from the
atmosphere, volcanic eruptions, a downward phase of the 11 - year solar cycle, and other impacts
over a
short time
period,» Cleugh says.
When you say «we're» cooling now, you must mean the troposphere
over some
short period of time and certianly less heat is flowing from ocean to
atmosphere during the current cool PDO.
Methane has a restricted lifetime in the
atmosphere, measured in decades, but while present in the air it has a greenhouse effect some 25 times that of CO2
over a 100 - year
period and higher values
over shorter periods.
The data and the statistical analysis does not provide the evidence that the so called «pause», a time
period with a lower trend estimate than the longer - term trend estimate, was more than just a
short - term fluctuation around the median warming trend, mostly due to
short - term unforced internal variability in the Earth system (and some contribution from decreasing solar activity and increased reflecting aerosols in the
atmosphere, counteracting the increased greenhose gas forcing to some degree), like the «acceleration»
over the 16 - year
period from 1992 to 2007 (e.g., UAH trend: 0.296 + / - 0.213 (2 sigma) deg.
A. Weather — condition of the bottom layer of the earth's
atmosphere in one place
over a
short period of time B.
But some scientists argue that the impact of methane gas should be calculated
over a
shorter time
period, because methane degrades quickly, and because gas drilling releases large quantities of methane into the
atmosphere all at once, likely concentrating and amplifying the effect.