Earth and Planetary Sciences
Africa
39%
Air Temperature
27%
Alkenone
32%
Atmospheric Circulation
17%
Atmospherics
31%
Boundary Condition
17%
California
20%
Climate Change
71%
Climate Modeling
71%
Climate Variation
27%
Data Assimilation
19%
Eastern Africa
36%
Eocene
57%
Foraminifera
15%
Grassland
12%
Greenhouse Gas
21%
Holocene
68%
Ice Sheet
29%
Indian Ocean
56%
Isotopic Composition
23%
Lacustrine Deposit
30%
Last Glacial
12%
Last Glacial Maximum
76%
Late Pleistocene
23%
Marine Isotope Stage
12%
Marine Sediment
22%
Methylation
11%
Miocene
12%
North America
15%
North Atlantic
16%
Northern Hemisphere
34%
Ocean Surface
13%
Paleocene
21%
Paleoclimate
94%
Paleotemperature
43%
Planetary Atmosphere
23%
Pleistocene
11%
Pliocene
46%
Sea Level
18%
Sea Surface Temperature
100%
Seasonality
18%
Sediment Core
19%
Speleothem
18%
Surface Cooling
12%
Time Series
17%
United States of America
16%
Vegetation
63%
Walker Circulation
14%
Warm Pool
63%
Water Column
14%
Keyphrases
Atmospheric Circulation
7%
Branched GDGTs
8%
Branched Glycerol Dialkyl Glycerol Tetraethers (brGDGTs)
34%
California Margin
10%
Climate Change
11%
Climate Sensitivity
13%
Climate Simulation
10%
Climate System
8%
Climate Variability
10%
Deglacial
12%
Early Eocene Climatic Optimum
10%
East Africa
10%
East African
8%
Eastern Pacific Warm Pool
8%
Glacial Change
7%
Global Database
31%
Holocene Temperature
7%
Homo Sapiens
12%
Horn of Africa
8%
Hydroclimate
29%
Hydroclimatic Variability
7%
Ice Sheet
14%
Indian Monsoon
10%
Indian Ocean
24%
Indo-Pacific Warm Pool
19%
Last Glacial Maximum
27%
Leaf Wax
7%
Microcosm
12%
Model Simulation
13%
Monsoon
14%
North American Monsoon
18%
Northern Hemisphere
12%
Paleocene-Eocene Thermal Maximum
12%
Paleoclimate
8%
Paleoclimate Records
14%
Paleotemperature
25%
Paleotemperature Proxy
10%
Pliocene Warmth
9%
Proxy Data
14%
Proxy Records
20%
Sea Surface Temperature
25%
Surface Cooling
12%
Temperature Proxy
10%
Temperature Sensitivity
10%
TEX86
10%
Tropical Climate
9%
Vegetation Change
7%
Ventilation
7%
Warm Pool
12%
Western Indian Ocean
7%