ANSWER :-
#13:-
Different greenhouse gases last in the atmosphere for different
duration, and they also absorb different amounts of heat.
The “global warming potential” of a GHG indicates the amount of
warming a gas causes over a given period of time (normally 100
years).
GWP is an index, with CO2 having the index value of 1, and the GWP
for all other GHGs is the number of times more warming they cause
compared to CO2. Example:- 1kg of methane causes 25 times more
warming over a 100 year period compared to 1kg of CO2, and so
methane as a GWP of 25.

From the table given above
GWP of methane - 25
GWP of N2O - 298
64 kg of methane = 64 x 25 = 1600 kg of CO2
800g of Nitrous oxide = 0.8 x 298 = 238.4 kg of CO2
So, total CO2 emission = 1600 + 238.4 = 1838.4 kg
#14:-
It is not scientifically possible to assign individual weather
events to the current climate change, however, it can be
statistically proven that global warming will increase the
probability of extreme weather events.
The direct consequences of man-made climate
change include:
The indirect consequences of climate change, which directly affect us humans and our environment, include:
the need for adaptation in all areas (e.g. agriculture,
forestry, energy, infrastructure, tourism, etc.)
As the global climate is a highly interconnected system that is
influenced by many different factors, the consequences usually
result in positive or negative feedback effects. This refers to
developments that are self-enhancing due to the occurrence of
certain conditions.
A common example is the ice-albedo feedback, which refers to the
melting of the polar caps. According to this, extensive ice
surfaces have a cooling effect on the global climate, as a high
proportion of radiation is reflected. As a result of the
global rise in the average temperature, however, these ice
surfaces begin to melt, the ice surfaces shrink and the amount of
reflected radiation is reduced. At the same time, the area of land
or ocean that has a significantly lower albedo will increase,
reflecting less radiation and thus intensifying the actual cause of
glacier melt.
Furthermore, scientists can calculate the so-called tipping points
of individual subsystems of the global climate. The higher
the global rise in temperature, the more the climate system is
affected, so that at a certain point, despite significant
efforts, a reversal in the process is no longer possible. Where
exactly these tipping points can be found, however, is currently
still unclear and can only be calculated with a great degree of
uncertainty. Such tipping points are expected for the melting of
the polar caps and for the stability of important ocean
currents
Global warming is an aspect of climate change, referring to
the long-term rise of the planet's temperatures. It is caused by
increased concentrations of greenhouse gases in the atmosphere,
mainly from human activities such as burning fossil fuels, and
farming.
So all of the above can be reasons of climate change in the long
term.
#15 :-
The Eight Millennium Development Goals are:
13 # A rice puddy produces 64.0kg methane and Goog of Nro. What is the total...
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