首页> 外文会议>Asian conference on remote sensing;ACRS 2007 >ESTIMATION OF TROPICAL FOREST BIOMASS FOR ASSESSMENT OF CARBON SEQUESTRATION USING REGRESSION MODELS AND REMOTE SENSING IN BERAU, EAST KALIMANTAN, INDONESIA
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ESTIMATION OF TROPICAL FOREST BIOMASS FOR ASSESSMENT OF CARBON SEQUESTRATION USING REGRESSION MODELS AND REMOTE SENSING IN BERAU, EAST KALIMANTAN, INDONESIA

机译:回归模型和遥感在印度尼西亚东加里曼丹省的热带森林中评估碳隔离的热带生物量

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Greenhouse gases play an important role on Earth's climate. These include water vapour, carbon dioxide, methane, nitrous oxide, and ozone. When sunlight reaches the surface of the Earth, some are absorbed and warm the Earth. In turn, the Earth emits long wave radiation towards the atmosphere, a fraction of which is absorbed by the greenhouse gases. The Greenhouse gases then emits long wave radiation both towards space and back to the Earth. The energy emitted downward further warms the surface of the Earth. The process of absorbing long wave radiation by the greenhouse gases and emitting it back resulting to more warming of the Earth's surface is called "greenhouse effect". When the concentration of greenhouse gasses in the atmosphere increased, temperature at the Earth's surface is also expected to increase. Climate models developed in the 90's have shown that global surface air temperature may increase by 1.4 °C to 5.8°C at the end of the century (IPCC, 2001; Rahmstorf and Ganopolski, 1999). Recent IPCC (2007) report predicted increase in temperature with more precision at 1.8 °C to 4 °C at the end of the century. Petit et al. (1999) has link temperature increase to increase in the concentration of CO_2 in the atmosphere.
机译:温室气体在地球的气候中发挥着重要作用。这些包括水蒸气,二氧化碳,甲烷,氧化亚氮和臭氧。当阳光到达地球表面时,有些人被吸收和温暖地球。反过来,地球向大气发出长波辐射,一小部分被温室气体吸收。温室气体然后发出长波辐射,既朝向空间又回到地球上。向下发出的能量进一步温暖了地球表面。通过温室气体吸收长波辐射的过程并将其发出回来导致地球表面的变暖被称为“温室效应”。当大气中温室气体的浓度增加时,地球表面的温度也会增加。在90年代开发的气候模型表明,世纪末全球表面空气温度可能会增加1.4°C至5.8°C(IPCC,2001; Rahmstorf和Ganopolski,1999)。最近的IPCC(2007)报告预测,在本世纪末的1.8°C至4°C时,预测温度的增加。 Petit等人。 (1999)链接温度升高以增加大气中CO_2的浓度。

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