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Observations of deep convective clouds as stable reflected light standard for climate research: AIRS evaluation

机译:深度对流云的观察为气候研究稳定反射光标准:Airs评估

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Changes of the order of 1 %/decade or less are expected in the tropical ocean cloud amount due to global warming. Since the ocean is very dark in the visible and near infrared region of the spectrum, a change in the Earth reflectance is equivalent to a measure of the change in the cloud cover. A reliable measurement of such a small change in the visible requires a reference source which is much more stable than 1 %/decade. A procedure is developed to use the sunlight reflected from Deep Convective Clouds (DCC) as a stable and readily available reference source for reflected light channels. The procedure uses the stability of the NIST traceable infrared radiometric calibration of the Atmospheric Infrared Sounder (AIRS) to create a stable DCC detection threshold, which assures a stable visible reflected reference signal. DCC are identified in the data as any IR footprint within ±30 degree latitude, where the brightness temperature in the 1231 cm~(-1) window channel is 210K or less. The 90%tile value of the observed visible signal is used as reference to minimize the effect of under-filling the footprint. Typically 2000 DCC are identified each day during the daylight part of the orbit. The stability uncertainty in the DCC reference signal measured from the first four years of AIRS data is 0.02%/year, I.e. 0.2%/decade. The stability of the procedure demonstrated with AIRS is thus already better than the 1 %/decade expected change in the cloud amount due to global warming. Extrapolated from four years to the expected 12 year lifetime of AIRS the trend uncertainty on the DCC measurements should decrease to 0.06%/decade. A 12 year record of the Earth reflectance stabilized with the DCC would allow for a very sensitive test of a change in the cloud amount.AIRS was launched on the EOS Aqua spacecraft in May 2002 into a 705 km polar sun-synchronous orbit with accurately maintained 1:30 PM ascending node. Essentially un-interrupted data are freely available since September 2002. The DCC are included in the AIRS Calibration Data Subset (ACDS).
机译:由于全球变暖,在热带海洋云金额中预期1%/十年或更低的顺序的变化。由于海洋在光谱的可见和近红外区域中非常暗,因此地球反射率的变化相当于云盖的变化的量度。可靠地测量可见的这种小变化需要参考源,其比1%/十年更稳定。开发了一种程序以使用从深度对流云(DCC)反射的阳光作为反射光通道的稳定且易于获得的参考源。该程序使用大气红外发声器(空气)的NIST可追踪红外辐射校准的稳定性来产生稳定的DCC检测阈值,该阈值确保了稳定的可见反射参考信号。 DCC在数据中被识别为±30度纬度的任何IR占地面积,其中1231cm〜(-1)窗口通道中的亮度温度为210k或更小。观察到的可见信号的90%瓦片值用作参考,以最大限度地减少填充占地面积的效果。通常,在轨道的日光部分期间每天识别2000年DCC。从烟囱数据的前四年测量的DCC参考信号中的稳定性不确定性为0.02%/年,即0.2%/十年。因此,由于全球变暖,空气所证明的程序的稳定性比云量的1%/十年的预期变化更好。从四年后推断到预期的12年终生的空气寿命,DCC测量的趋势不确定性应减少到0.06%/十年。与DCC稳定的地球反射率的12年记录将允许对云量的变化进行非常敏感的测试。在2002年5月,EOS Aqua SpaceCraft在EOS Aqua SpaceCraft上发布了705公里的极性太阳同步轨道,精确维护下午1:30升序节点。自2002年9月以来,基本上无法中断数据可自由使用。DCC包含在Airs校准数据子集(ACD)中。

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