what is global warming
what is global warming
What is the annual increasing rate of global temperature ?
In the equatorial zone it seems that nothing happens, where the phenomena of boy and girl do to change the weather in winter periods of the summer becomes what happens?
el aumento de la temperatura puede ser el calentamiento de efecto invernadero, observemos las variables climáticas para ver las causas de esto. empecemos por el Himalaya. que ya retrocedido mas de 5 km y se contraen mucho por año, pueden desaparecer en el 2035 causando así problemas. Puesto que esto puede causar inundaciones y debilitamiento de los suelos.
One of great indicators are unpredictable seasons e.g characterized by extreme weather floods, extreme coldness and hotness.
What is Climate Change?
Global climate change is one of the most serious challenges facing us today.
The observed increase in global mean standard temperature may be the key global indicator of greenhouse warming, but it is far from being the only tangible sign of climate change during the 20th century.
Here, we take a brief look at the growing body of evidence that many different climate variables, as well as physical and biological systems around the world, have been affected by recent climate warming.
The six examples collected will give you a flavour of the sorts of reports that are now emerging from research programmes. Click on the links below for more information.
The Khumbu Glacier in the Himalaya (on a popular climbing route to the summit of Mount Everest) has retreated by over 5 km since 1953.
In the central and eastern Himalaya, glaciers are contracting at an average rate of 15m per year, and could be gone by 2035 if this trend continues - with serious implications for populations who depend on glacial meltwater for drinking supplies, etc.
Meanwhile, glacial lakes are swelling in Bhutan, increasing the risk of catastrophic flooding downstream.
Most of the state of Alaska is underlain by permafrost (permanently frozen soil). Thawing permafrost is causing the ground to subside (by 4-10m in some places), undermining buildings, roads and other infrastructure.
In some coastal areas, wave action is undermining cliffs softened by permafrost melt, increasing the risk of flooding for native communities. In the interior, forests of spruce and birch are taking on a ‘drunken’ appearance on softening ground, and trees are dying as they succumb to waterlogged conditions.
Rising sea levels in the Chokoria Sundarbans of Bangladesh have flooded about 7500 hectares of coastal mangrove forest during the past three decades.
Global sea-level rise is aggravated by substantial deltaic subsidence in the area due mainly to human activities, such as reduced sediment supply following dam construction upstream for irrigation schemes, and the over-extraction of groundwater.
The average flowering date of 385 British plant species has advanced by 4.5 days during the 1990s compared with the previous four decades. 16% of the species flowered 15 days earlier on average.
Over a 20-year period (between 1968-72 and 1988-91), many bird species have extended the northern margins of their breeding ranges in the UK by an average of 19 km.
A reduction in dry-season mists in the Monteverde Cloud Forest, Costa Rica due to warmer Pacific Ocean temperatures has been linked to the disappearance of 20 species of frogs and toads, upward shifts in the ranges of mountain birds, and declines in lizard populations.
Adélie penguin populations in the Antarctic peninsula have shrunk by 33% over the past 25 years in response to declines in their winter sea-ice habitat. Adélies depend on sea ice as a resting and feeding platform.
They are being replaced by gentoo penguins (a sub-Antarctic species that has begun to migrate towards the pole) which thrive in open water.