Results 171 to 180 of about 4,738 (245)

Climate impacts from North American boreal forest fires. [PDF]

Nat Geosci
van Gerrevink MJ, Veraverbeke S, Cooperdock S, Potter S, Zhong Q, Moubarak M, Virkkala AM, Goetz SJ, Mack MC, Randerson JT, Schutgens N, Turetsky MR, van der Werf GR, Rogers BM.   +13 more
europepmc   +1 more source

Spatial Patterns of Glacier‐Wetland Hydrological Connectivity in the Rapidly Deglaciating Peruvian Andes

Earth's Future, Volume 14, Issue 6, June 2026.
Abstract High‐altitude wetlands are critical ecosystems that store water, regulate downstream flows, and sustain biodiversity. Their persistence is tightly linked to continuous water inputs from precipitation, groundwater, snow and glacier melt, making them highly vulnerable to climate‐driven shifts in mountain hydrology. Rapid glacier retreat, altered
D. Xuan, R. Becker, M. Vargas Valverde, B. J. Davies, J. C. Ely, O. King, N. Montoya, C. Onof, A. C. Ross, W. Buytaert   +9 more
wiley   +1 more source

Non-Abrupt Vegetation Changes due to Altered Nutrient Balance Make Complex Scale-Dependent Warming and Cooling Effects. [PDF]

Glob Chang Biol
Hanggara B, El-Madany T, Carrara A, Moreno G, Gonzalez-Cascon R, Burchard-Levine V, Martin MP, Metzger S, Hildebrandt A, Reichstein M, Lee SC.   +10 more
europepmc   +1 more source

Mastcam‐Z Spectrophotometric Properties of Materials at the Van Zyl Overlook, Jezero Crater

Journal of Geophysical Research: Planets, Volume 131, Issue 6, June 2026.
Abstract During Sols 63–65 of Mars 2020, Mastcam‐Z multispectral (442–1022 nm) images were acquired at Van Zyl Overlook (VZO), spanning phase angles from ∼0° to 150°, to model photometric parameters for seven surface units. These units included rocks, soils, regolith, and rover tracks near the Jezero landing site.
B. Margara, J. R. Johnson, A. G. Hayes, M. T. Lemmon, W. M. Grundy, J. F. Bell III, M. N. Barrington   +6 more
wiley   +1 more source

Asymmetric global urban cooling potential demands accelerated and context-specific actions. [PDF]

Nat Commun
Ding X, Fan Y, Zhao Y, Ürge-Vorsatz D, Ge J, Carmeliet J.   +5 more
europepmc   +1 more source

Monitoring land surface albedo and vegetation dynamics using high spatial and temporal resolution synthetic time series from Landsat and the MODIS BRDF/NBAR/albedo product. [PDF]

Int J Appl Earth Obs Geoinf, 2017
Wang Z, Schaaf CB, Sun Q, Kim J, Erb AM, Gao F, Román MO, Yang Y, Petroy S, Taylor JR, Masek JG, Morisette JT, Zhang X, Papuga SA.   +13 more
europepmc   +1 more source

Estimation of Land Surface Albedo from GCOM-C/SGLI Surface Reflectance

Estimation of Land Surface Albedo from GCOM-C/SGLI Surface Reflectance
This paper examines algorithms for estimating terrestrial albedo from the products of the Global Change Observation Mission – Climate (GCOM-C)/Second-generation Global Imager (SGLI), which was launched in December 2017 by the Japan Aerospace Exploration Agency.
openaire  

Martian Proton Albedo as Signature of Near‐Surface Water

Journal of Geophysical Research: Planets, Volume 131, Issue 6, June 2026.
Abstract Understanding the Martian soil water budget is crucial not only for in situ resource utilization in future human missions to Mars, but also for reconstructing the geological and climatic history of the planet, as well as to assess the potential of ancient or even present microbial life.
Jan Leo Löwe, Robert F. Wimmer‐Schweingruber, Salman Khaksari, Sven Löffler, Sergey Nikiforov, Maya Djachkova, Jingnan Guo, Gabin Charpentier, Bent Ehresmann, Donald M. Hassler, Daniel Matthiä, Thomas Berger, Günther Reitz, Cary Zeitlin   +13 more
wiley   +1 more source

Accelerated land surface greening caused by earlier permafrost thawing. [PDF]

Nat Commun
Hua H, Wang J, Zohner CM, Peñuelas J, Ran Y, Wu C.   +5 more
europepmc   +1 more source

Spectral Characterization of CO2‐H2O Ice Layering Under Controlled Mars Polar Conditions as Laboratory Analogs for Seasonal Cap Activity

Journal of Geophysical Research: Planets, Volume 131, Issue 6, June 2026.
Abstract Seasonal CO2 and H2O ice blanket the Martian polar caps, and their spectral contributions mix during seasonal evolution. Particularly in late northern winter, the spectral signature of H2O ice obscures that of CO2 ice. Using the MARVIN chamber at York University, we produced controlled analogs of layered polar ice under Mars‐like pressure (∼6 ...
Jamie A. Isen, Andrej Stojanovic, Wendy M. Calvin, Isaac B. Smith   +3 more
wiley   +1 more source