Posts Tagged ‘albedo’

Climate Models: Albedo, Earthshine

Thursday, November 5th, 2009

NASA

Measuring Earthshine: How New Terra Data are Improving Weather and Climate Forecast Models

A sensor aboard NASA’s Terra satellite is helping scientists map how much sunlight the Earth’s surface reflects back up into the atmosphere, and this new detailed information should help to greatly improve weather and forecast models.

The Moderate Resolution Imaging Spectroradiometer (MODIS) now routinely provides daily global and local measurements of albedo, or the total amount of light reflected from Earth’s surface out to space. These precise data may allow scientists to better understand and predict how various surface features absorb and reflect solar radiation, which influence both short-term weather patterns and longer-term climate trends.

American Meteorological Society

Land surface albedo is a critical parameter affecting the earth’s climate. For many general circulation models (GCMs), both visible (0.4–0.7 μm) and near-infrared (0.7–5.0 μm) albedos are needed, whereas the surface energy balance studies typically require broadband shortwave (0.25–5.0 μm) albedo. Although surface albedo has been routinely observed for a long time and different approaches have been explored, a global map of surface albedo with high accuracy is not simply available right now. It has been well recognized that surface albedo is among the main radiative uncertainties in current climate modeling. Most GCMs are still using prescribed fields of surface albedo that are often 5%–15% in error from place to place and time to time.

More than CO2? Reflective or albedo effects also?

Wednesday, November 4th, 2009

The earth is getting hotter – or is it not? Has the Sun increased it´s shining during the last 150 years?

Our understanding of the the climate problem is not complete and will not be solved by focusing on CO2 alone. The calculation of carbon neutrality has to take into account the fact that the sun shines on the earth with a force of 1350 Wm2, whereas the effect due to burning fossil fuel is only 1-2 Wm2. As an example massive removal of forests in temperate zones will cool the earth, while deforestation in the tropics will increase the temperature.

Scientists haven’t been able to quantify accurately what the effect of CO2 on temperature is. Reduce CO2 or maybe it is just as effective to alter the reflective properties or color of the earth?

The albedo or reflective properties of the earth is an important concept in climatology and must be accounted for in the models used.

The albedo of an object is the extent to which it diffusely reflects light from light sources – in the case of the earth the Sun. It is a unitless measure between 0 and 1 indicative of a surface’s or body’s diffuse reflectivity. The word is derived from Latin albedo “whiteness”.

“Terrestrial albedo: Albedos of typical materials in the visible light range from up to 90% for fresh snow, to about 4% for charcoal, one of the darkest substances. Deeply shadowed cavities can achieve an effective albedo approaching the zero of a blackbody. When seen from a distance, the ocean surface has a low albedo, as do most forests, while desert areas have some of the highest albedos among landforms. Most land areas are in an albedo range of 0.1 to 0.4. The average albedo of the Earth is about 30%. This is far higher than for the ocean primarily because of the contribution of clouds. ” (Wikipedia)

Human activities have changed the albedo (e.g. forest clearance, farming) around the globe. Quantification of this effect on the global scale is difficult.

An example of the albedo effect is the snow-temperature feedback: a snow-covered area warms and the snow melts, the albedo decreases, more sunlight is absorbed, the temperature tends to increase. If snow forms, a cooling cycle happens. The intensity of the albedo effect depends on the amount of sunshine – it can be potentially very large in the tropics.

The Earth’s surface albedo is regularly estimated via Earth observation satellite sensors.

The Earth’s average surface temperature due to its albedo and the greenhouse effect is currently about 15°C. Based on theoretical models it has been estimated that for the frozen (more reflective) planet the average temperature is below -40°C.  If all continents only were completely covered by glaciers the mean temperature would be about 0°C. The simulation for the more absorptive aquaplanet shows the average temperature close to 27°C.

There are CO2 critics: The journalist Christopher Monckton (among others) is critical of the theory of man-made causes for climate change and the stated scope of it – it is unlikely to prove catastrophic. He has criticized the Intergovernmental Panel on Climate Change (IPCC), their interpretation of the Medieval Warm Period, the “hockey stick” model. He supports the solar variation theory as a possible explanation of global warming. He states that Gore and the IPCC has systematically falsified and exaggerated the evidence for global warming.

Scientists are sceptical as well: Ferenc Miskolcz (among others) says that the Earth’s atmosphere dynamically keeps its greenhouse effect right at its critical value, regardless of our continuing CO2 emissions, regardless of any change in atmospheric CO2 concentration in the past ten thousand years. Miskolczi’s dynamic constraint keeps the greenhouse effect “climatically saturated”: emitting CO2 into the air cannot increase the normalized greenhouse factor g because any impact of human addition of CO2 is dynamically countered by about 1% decrease of the main greenhouse gas water vapor (moisture) in the atmosphere.

The aim must be to check, control or reduce total warming. Comprehensive models with a good combination of empirical and theoretical science must be established.