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The India-Eurasia continental collision zone provides a spectacular example of active mountain building and climatic forcing. In order to quantify the critically important process of mass removal, I analyzed spatial and temporal precipitation patterns of the oscillating monsoon system and their geomorphic imprints. I processed passive microwave satellite data to derive high-resolution rainfall estimates for the last decade and identified an abnormal monsoon year in 2002. During this year, precipitation migrated far into the Sutlej Valley in the northwestern part of the Himalaya and reached regions behind orographic barriers that are normally arid. There, sediment flux, mean basin denudation rates, and channel-forming processes such as erosion by debris-flows increased significantly. Similarly, during the late Pleistocene and early Holocene, solar forcing increased the strength of the Indian summer monsoon for several millennia and presumably lead to analogous precipitation distribution as were observed during 2002. However, the persistent humid conditions in the steep, high-elevation parts of the Sutlej River resulted in deep-seated landsliding. Landslides were exceptionally large, mainly due to two processes that I infer for this time: At the onset of the intensified monsoon at 9.7 ka BP heavy rainfall and high river discharge removed material stored along the river, and lowered the baselevel. Second, enhanced discharge, sediment flux, and increased pore-water pressures along the hillslopes eventually lead to exceptionally large landslides that have not been observed in other periods. The excess sediments that were removed from the upstream parts of the Sutlej Valley were rapidly deposited in the low-gradient sectors of the lower Sutlej River. Timing of downcutting correlates with centennial-long weaker monsoon periods that were characterized by lower rainfall. I explain this relationship by taking sediment flux and rainfall dynamics into account: High sediment flux derived from the upstream parts of the Sutlej River during strong monsoon phases prevents fluvial incision due to oversaturation the fluvial sediment-transport capacity. In contrast, weaker monsoons result in a lower sediment flux that allows incision in the low-elevation parts of the Sutlej River.
Muster globaler anthropogener CO₂-Emissionen : sozio-ökonomische Determinanten und ihre Wirkung
(2004)
Die wesentlichen sozio-ökonomischen Prozesse, die die vermehrten anthropogenen CO₂-Emissionen verursachen, können durch die Determinanten Bevölkerung, Wohlstand (Bruttoinlandsprodukt pro Kopf) und Technologie (Energie- und Kohlenstoffintensität) vereinfacht beschrieben werden. Der Einfluss dieser Determinanten auf die Emissionsänderungen ist nicht für alle Länder der Erde gleich. Zeitreihen der CO₂-Emissionen aus der Verbrennung fossiler Energieträger, der Bevölkerung, des Bruttoinlandsproduktes und des Primärenergieverbrauches von 121 Ländern bilden die Grundlage für das entwickelte statistische Verfahren zur schrittweisen Informationsverdichtung, mit dem der gesamte Datenraum zu 6 energiewirtschaftlichen Ländertypen schrittweise zusammengefasst wird. Zur Beschreibung dieser Ländertypen wird mit Hilfe der Dekompositionsanalyse der Einfluss der Bevölkerungs-, der Wohlstands- und der Technologiekomponenten an den Emissionsänderungen quantifiziert. Die Ländertypen können vereinfacht als Repräsentanten unterschiedlicher Entwicklungsstufen und -richtungen angesehen werden. Sie bilden unter anderem eine Grundlage für die Weiterentwicklung und Kalibrierung regionalisierter makro-ökonomischer Modelle zu den sozio-ökonomischen Hintergründen der vermehrten anthropogenen CO₂-Emissionen.