<?xml version="1.0" encoding="UTF-8"?><rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcq="http://purl.org/dc/terms/"><records count="1" morepages="false" start="1" end="1"><record rownumber="1"><dc:product_type>Dataset</dc:product_type><dc:title>Saddle soil temperature and moisture, 2024 - ongoing.</dc:title><dc:creator>Morse, Jennifer F; LTER, Niwot Ridge</dc:creator><dc:corporate_author/><dc:editor/><dc:description>In rugged mountain terrain, microclimate variation may provide
 refugia that buffer the effects of climate change. We expect that
 complex terrain causes microsite variation in surface and subsurface
 temperature and soil moisture across hillslopes, thus mediating the
 extent to which organisms are exposed to warming conditions.
 Further, we expect that hillslope position will determine the
 microclimate that regulates ecological and biogeochemical
 responses.</dc:description><dc:publisher>Environmental Data Initiative</dc:publisher><dc:date>2025-02-22</dc:date><dc:nsf_par_id>10632770</dc:nsf_par_id><dc:journal_name/><dc:journal_volume/><dc:journal_issue/><dc:page_range_or_elocation/><dc:issn/><dc:isbn/><dc:doi>https://doi.org/10.6073/pasta/a1ac88389c35f1e23c3c354b20754c5d</dc:doi><dcq:identifierAwardId>2224439</dcq:identifierAwardId><dc:subject/><dc:version_number/><dc:location/><dc:rights/><dc:institution/><dc:sponsoring_org>National Science Foundation</dc:sponsoring_org></record></records></rdf:RDF>