The ocean s overall role in climate
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- Garey Barker
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1 The ocean s overall role in climate - moderates climate in time (diurnally, annually) - redistributes heat spatially in the largescale ocean circulation - lower albedo (sea ice higher albedo) - dry atmosphere has no clouds (smaller greenhouse effect) 1
2 The oceans moderates climate The heat capacity of the ocean is 100 times greater than that of land Effective heat capacity of the ocean (atmosphere) is that of a water body of m (3 m) depth 2
3 Two coastal cities: San Francisco 38ºN, New York 41ºN 3
4 NH 60% oceans SH 80% oceans 4
5 Damping of climate variability of the ocean 5
6 Ocean heat transport 6
7 Ocean heat transport 7
8 Source: Dommenget (2014) 8
9 Ocean heat transport 9
10 Ocean conveyor belt Source:Vallis (2012) Climate and the oceans 10
11 Atmosphere heat transport Low latitudes Hadley Cell Midlatitudes weather systems 11
12 12
13 Forced and unforced climate variability 1. Paleo climate variability (ice ages) 13
14 Natural climate variability Volcanic eruptions (forced) Aerosols and greenhouse gases (forced) Solar variability (Sunspot activity, orbital parameters) (forced) Tectonic changes Internal (=unforced) variability generated by the nonlinear dynamics of the climate system Anthropogenic impact on climate Anthropogenic emission of greenhous gases and aerosols (forced) 14
15 Präkambrium 3.5 Mrd first forms of life Source: 15
16 Climate (proxy) data 1. Thermometer measurements Source: Dommenget (2014) 16
17 Source: Dommenget (2014) 17
18 Climate (proxy) data 1. Thermometer measurements Source: Dommenget (2014) 18
19 Climate (proxy) data 1. Thermometer measurements Data area coverage over land (CRUTEMP) and oceans (HADISST) 19 Source: Dommenget (2014)
20 Climate (proxy) data 1. Thermometer measurements Cold ocean warm land pattern Source: Dommenget (2014) 20
21 Climate (proxy) data 1. Thermometer measurements UK ships measured in the Atlantic, US ships in the Pacific Source: Dommenget (2014) 21
22 Climate (proxy) data 2. Climate proxies: tree rings Summer temperature, dependence on the region Source: Dommenget (2014) 22
23 Climate (proxy) data 3. Climate proxies: ice cores δ O 18 Antarctic ice sheet (4 km) very old (1 mio years), O18 isotope ratios depend on the water masses (surrounding oceans) and atm temperatures that produce the precip, air bubbles (atm chem composition) Source: Dommenget (2014) 23
24 Climate (proxy) data 4. Climate proxies: corals Proxy of SST in shallow waters < 5m, many thousand years Source: Dommenget (2014) 24
25 Climate (proxy) data 5. Climate proxies: ice borehole temperatures Temp from the days when the ice layer is formed, many thousand years Source: Dommenget (2014) 25
26 Several climate indicators, track fossils, many million years Climate (proxy) data 6. Climate proxies: sediments Source: Dommenget (2014) 26
27 Climate (proxy) data Distribution of climate proxy data Source: Dommenget (2014) 27
28 Climate history 1. The last 2000 years Source: Dommenget (2014) 28
29 Hockey stick Climate of the past 2000 years relatively stabile, variability caused by internal variability with some impact of sun spot and volcanic activities Source: 29
30 Source: 30
31 Climate history 1. The last 2000 years Reconstruction of the northern hemisphere temperature Source: Dommenget (2014) 31
32 Source: 32
33 (Source: Luterbacher et al. 2016) Climate history 1. The last 2000 years
34 Climate history 2. The last years Source: Dommenget (2014) 34
35 Präkambrium 3.5 Mrd first forms of life Source: 35
36 Source: 36
37 Climate history 3. The last years (ice ages, Milankovitch cycles) Source: Dommenget (2014) 37
38 Präkambrium 3.5 Mrd first forms of life Source: 38
39 Climate history 3. The last years (ice ages, Milankovitch cycles) Dominated by big ice age cycles (short interglacials, long glacials), global extent, global temp difference 3K, some periods are 1-2 K warmer than today Source: Dommenget (2014) 39
40 Climate history Vostock ice core drilling site Thickest ice sheet, no drift, no snow, oldest ice Source: Dommenget (2014) 40
41 Climate history 3. The last years (ice ages, Milankovitch cycles) Source: Dommenget (2014) 41
42 Climate history 3. The last years (ice ages, Milankovitch cycles) Source: Dommenget (2014) 42
43 Causes of ice ages Reconstruction of the global temperatures during the last ice age maximum Source: Dommenget (2014) 43
44 Causes of ice ages Partly internal natural and external climate variabilty, including some important feedbacks Most important driver: variations in the Earth s orbit (Milankovitch cycles) Glacier feedbacks (ice albedo, water vapor, altitude cooling, atmospheric circulation) Other feedbacks: CO 2 uptake (cold oceans can take up more CO 2 ), land vegetation 44
45 Causes of ice ages Source: Dommenget (2014) 45
46 Source: 46
47 Source: 47
48 Causes of ice ages: orbital forcings (Milankovitch Cycles) cause mostly a redistribution of incoming radiation between latitudes and seasons (regional changes up to 50 Wm -2 over 10 kyr) S 0 =0.7 Wm o No effect if there is no excentricity and obliquity Source: 48
49 Causes of ice ages Source: 49
50 Causes of ice ages Source: Dommenget (2014) 50
51 Source: 51
52 Causes of ice ages Source: Dommenget (2014) 52
53 53
54 Open questions Shift Why is the year period soo strong and other frequencies not? Temperature spectrum looks like red noise 54
55 Causes of ice ages Source: Dommenget (2014) 55
56 Cause of ice ages Power spectrum of different ice core records 56
57 Climate history 4. The last 500 million years On time scales longer than 1 million years ago geography starts to vary (most recent event: south polar position of Antarctica, cooling) Source: Dommenget (2014) 57
58 Präkambrium 3.5 Mrd first forms of life Source: 58
59 Climate history 4. The last 500 million years Source: Dommenget (2014) 59
60 Source: 60
61 Source: 61
62 62
63 Präkambrium 3.5 Mrd first forms of life Source: 63
64 Climate history 4. The last 500 million years Source: Dommenget (2014) 64
65 Climate history 4. The last 500 million years Source: Dommenget (2014) 65
66 Climate history 4. The last 500 million years Source: Dommenget (2014) 66
67 Source: 67
68 Climate history 4. The last 500 million years Source: Dommenget (2014) 68
69 Climate history 4. The last 500 million years Source: Dommenget (2014) 69
70 Präkambrium Schneeball-Erde- Vereisung, Großkontinent Rodina, Verwitterung 2.9 Mrd Pangoa ice age 3.5 Mrd first forms of life Source: 70
71 Forced and unforced climate variability 2. Global warming caused by anthropogenic greenhouse gas emissions 71
72 Change in mean temperature compared to Source: 72
73 Source:Vallis: Climate and the oceans (2012) 73
74 Source:Vallis: Climate and the oceans (2012) 74
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