跳至主要内容

MODIS-Derived Nighttime Arctic Land-Surface Temperature Nascent Trends and Non-Stationary Changes

Read full paper at:
http://www.scirp.org/journal/PaperInformation.aspx?PaperID=47223#.VFwy2mfHRK0

Arctic nighttime land-surface temperatures derived by the Moderate Resolution Imaging Spectroradiometer (MODIS) sensors onboard the NASA Terra and Aqua satellites are investigated. We use the local equator crossing times of 22:30 and 01:30, respectively, in the analysis of changes, trends and variations on the Arctic region and within 120° sectors. We show increases in the number of days above 0°C and significant increase trends over their decadal periods of March 2000 through 2010 (MODIS Terra) and July 2002 through 2012 (MODIS Aqua). The MODIS Aqua nighttime Arctic land-surface temperature change, +0.2°C ± 0.2°C with P-value of 0.01 indicates a reduction relative to the MODIS Terra nighttime Arctic land-surface temperature change, +1.8°C ± 0.3°C with P-value of 0.01. This reduction is a decadal non-stationary component of the Arctic land-surface temperature changes. The reduction is greatest, -1.3°C ± 0.2°C with P-value of 0.01 in the Eastern Russia— Western North American sector of the Arctic during the July 2002 through 2012.
Cite this paper
Muskett, R. (2014) MODIS-Derived Nighttime Arctic Land-Surface Temperature Nascent Trends and Non-Stationary Changes. American Journal of Climate Change, 3, 169-177. doi: 10.4236/ajcc.2014.32016
 

[1] Mannstein, H. (1987) Surface Energy Budget, Surface Temperature and Thermal Inertia. In: Vaughan, R.A. and Reidel, D., Eds., Remote Sensing Applications in Meteorology and Climatology, Reidel Publishing Co., Dordrecht, 391-410.
[2] Wan, Z. (1999) MODIS Land-Surface Temperature Algorithm Theoretical Basis Document (LST ATBD) Version 3.3, National Aeronautics and Space. US Department of Commerce, Washington DC.
[3] Rowland, J.C., Jones, C.E., Altmann, G., Bryan, R., Crosby, B.T., Geernaert, G.L., Hinzman, L.D., Kane, D.L., Lawrence, D.M., Mancino, A., Marsh, P., McNamara, J.P., Romanovsky, V.E., Toniolo, H., Travis, B.J., Trochim, E. and Wilson, C.J. (2010) Arctic Landscapes in Transition: Responses to Thawing Permafrost. EOS Transactions of The American Geophysical Union, 91, 229-230.
http://dx.doi.org/10.1029/2010EO260001
[4] Jorgenson, M.T., Romanovsky, V.E., Harden, J., Shur, Y.L., O’Donnell, J., Schuur, T. and Kanevskiy, M. (2010) Resilience and Vulnerability of Permafrost to Climate Change. Canadian Journal of Forest Research, 40, 1219-1236.
http://dx.doi.org/10.1139/X10-060
[5] Grosse, G., Marchenko, S., Romanovsky, V., Wickland, K.P., French, N., Waldrop, M., Bourgeau-Chavez, L., Striegl, R., Harden, J., Turetsky, M., McGuire, A.D., Camill, P., Tarnocai, C., Frolking, S., Schuur, E. and Jorgenson, T. (2011) Vulnerability of High Latitude Soil Organic Carbon in North America to Disturbance. Journal Geophysical Research, 116, Article ID: G00K06.
http://dx.doi.org/10.1029/2010JG001507
[6] Houghton, R.A., Davidson, E.A. and Woodwell, G.M. (1998) Missing Sinks, Feedbacks, and Understanding the Role of Terrestrial Ecosystems in the Global Carbon Balance. Global Biogeochemical Cycles, 12, 25-34.
http://dx.doi.org/10.1029/97GB02729
[7] Muskett, R.R. (2013) MODIS-Derived Arctic Land-Surface Temperature Trends. Atmospheric and Climate Science, 3, 55-60.
http://dx.doi.org/10.4236/acs.2013.31008
[8] Xiong, X.X., Chiang, K.F., Wu, A.S., Barnes, W.L., Guenther, B. and Salomonson, V.V. (2008) Multiyear On-Orbit Calibration and Performance of Terra MODIS Thermal Emissive Bands. IEEE Transaction on Geoscience and Remote Sensing, 46, 1790-1803.
http://dx.doi.org/10.1109/TGRS.2008.916217
[9] Parkinson, C.L., Ward, A. and King, M.D. (2006) Earth Science Reference Handbook: A Guide to NASA’s Earth Science Program and Earth Observing Satellite Missions. In: Parkinson, C.L., Ward, A. and King, M.D., Eds., Earth Science Reference Handbook, National Aeronautics and Space Administration, US Department of Commerce, Washington DC, 1-6, 73-88, 225-227.
[10] L’Ecuyer, T.S. and Jiang, J.H. (2010) Touring the Atmosphere Aboard the A-Train. Physics Today, 63, 36-41.
[11] Xiong, X.X., Sun, J.Q. and Barnes, W. (2008) Intercomparison of On-Orbit Calibration Consistency between Terra and Aqua MODIS Reflective Solar Bands Using the Moon. IEEE Geoscience and Remote Sensing Letters, 5, 778-782.
http://dx.doi.org/10.1109/LGRS.2008.2005591
[12] Wan, Z. (2008) New Refinements and Validation of MODIS Land-Surface Temperature/Emissivity Products. Remote Sensing Environment, 112, 59-74.
http://dx.doi.org/10.1016/j.rse.2006.06.026
[13] Coll, C., Wan, Z. and Galve, G.M. (2009) Temperature-Based and Radiance-Based Validations of the V5 MODIS Land Surface Temperature Product. Journal Geophysical Research, 114, Article ID: D20102.
[14] Wang, W., Liang, S. and Meyers, T. (2008) Validating MODIS Land Surface Temperature Products Using Long-Term Nighttime Ground Measurements. Remote Sensing Environment, 112, 623-635.
[15] Hall, D.K., Box, J.E., Casey, K.A., Hook, S.J., Shuman, C.A. and Steffen, K. (2008) Comparison of Satellite-Derived and In-Situ Observations of Ice and Snow Surface Temperatures over Greenland. Remote Sensing Environment, 112, 3739-3749.
http://dx.doi.org/10.1016/j.rse.2008.05.007
[16] Hachem, S., Duguay, C.R. and Allard, M. (2011) Comparison of MODIS-Derived Land Surface Temperatures with Near-Surface Soil and Air Temperature Measurements in the Continuous Permafrost Terrain. The Cryosphere Discussion, 5, 1583-1625.
http://dx.doi.org/10.5194/tcd-5-1583-2011
[17] Weatherhead, B., Tanskanen, A. and Stevermer, A. (2005) Factors Affecting Surface Ultraviolet Radiation Levels in the Arctic. Chapter 5.4. In: ACIA, Ed., Arctic Climate Impact Assessment, Cambridge University Press, 159-164.
[18] Usoskin, I.G. (2008) A History of Solar Activity over Millennia. Living Reviews in Solar Physics, 5, 1-88.
http://www.livingreviews.org/lrsp-2008-3
[19] Stephenson, F.R. (1988) Solar Variability from Historical Records. In: Stephenson, F.R. and Wolfendale, A.W., Eds., NATO ASI Series C, Mathematical and Physical Sciences Vol. 236, Kluwer Academic Publishers, Springer, New York, 109-129.
[20] Soon, W.W.-H. (2009) Solar Arctic-Mediated Climate Variation on Multidecadal to Centennial Timescales: Empirical Evidence, Mechanistic Explanations, and Testable Consequences. Physical Geography, 30, 144-184.
http://dx.doi.org/10.2747/0272-3646.30.2.144
[21] Soon, W.W.-H. (2005) Variable Solar Irradiance as a Plausible Agent for Multidecadal Variations in the Arctic-Wide Surface Air Temperature Record of the Past 130 Years. Geophysical Research Letters, 32, Article ID: L16712.
http://dx.doi.org/10.1029/2005GL023429
[22] Usoskin, I.G., Solanki, S.K. and Kovaltsov, G.A. (2007) Grand Minima and Maxima of Solar Activity: New Observational Constraints. Astronomy and Astrophysics, 471, 301-309.
http://dx.doi.org/10.1051/0004-6361:20077704
[23] Scafetta, N. and West, B.J. (2006) Phenomenological Solar Signature in 400 Years of Reconstructed Northern Hemisphere Temperature Record. Geophysical Research Letters, 33, Article ID: L17718.
http://dx.doi.org/10.1029/2006GL027142
[24] Tinsley, B.A. and Yu, F. (2004) Atmospheric Ionization and Clouds as Links between Solar Activity and Climate. In: Judit, M., Fox, R., Frohlich, C., Hudson, H.S., Kuhn, J., McCormack, J., North, G., Sprigg, W. and Wu, S.T., Eds., Solar Variability and Its Effects on Climate, AGU Geophysical Monograph Series, No. 141, 321-339.                   eww141107lx

评论

此博客中的热门博文

Electron Spin and Proton Spin in the Hydrogen and Hydrogen-Like Atomic Systems

Read full paper at: http://www.scirp.org/journal/PaperInformation.aspx?PaperID=52202#.VIj7tMnQrzE Author(s) Stanisław Olszewski * Affiliation(s) Institute of Physical Chemistry, Polish Academy of Sciences, Warsaw, Poland . ABSTRACT The mechanical angular momentum and magnetic moment of the electron and proton spin have been calculated semiclassically with the aid of the uncertainty principle for energy and time. The spin effects of both kinds of the elementary particles can be expressed in terms of similar formulae. The quantization of the spin motion has been done on the basis of the old quantum theory. It gives a quantum number n = 1/2 as the index of the spin state acceptable for both the electron and proton ...

Incorporation of High-Altitude Balloon Experiment in High School Science Classrooms

High-altitude balloon is a balloon, filled usually with helium or hydrogen that ascends into an area called “near space” or stratosphere. The most common type of high-altitude balloons are weather balloons. Other purposes include use as a platform for experiments in the upper atmosphere. Modern balloons generally contain electronic equipment such as radio transmitters, cameras, or satellite navigation systems, such as GPS receivers. The mission of the High-Altitude Balloon Experiment (HABE) is to acquire supporting data, validate enabling technologies, and resolve critical acquisition, tracking, and pointing (ATP) and fire control issues in support of future space-based precision pointing experiments. The use of high-altitude balloons offers a relatively low-cost, low-vibration test platform, a recoverable and reusable payload, worldwide launch capability, and a 'near- space' emulation of the future space systems operational scenarios. More recently, several university...

Fermented Brown Sugar Residue Prolongs the Caenorhabditis elegans Lifespan via DAF-16

Fermented brown sugar residue (FBSR) is generated in the course of purifying biomass ethanol from the yeast fermentation products of brown sugar. It contains abundant nutrition and is used in various industrial applications including as fertilizer and feed. Meanwhile, brown sugar has attracted attention as a health food and is thought to prevent cardiovascular diseases, hypertension, and brain stem diseases. Furthermore, polyphenol, contained in brown sugar, reduces oxidative stress and inhibits glucose absorption. DAF-16 is a transcription factor regulated downstream of the insulin signaling pathway and is one of the main factors contributing to aging and lifespan in C. elegans . Therefore, to determine the precise roles of the DAF-16 transcription factor in stress tolerance and life span, it is necessary to elucidate the signaling pathways involved in DAF-16 activation. This study was designed to elucidate the molecular mechanisms controlling the physiological stress toleran...